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HomeMy WebLinkAbout02-WesternArcheologicalReptREPORT ON THE FILE SEARCH AND THE CLASS III CULTURAL RESOURCE INVENTORY FOR A SENSITIVE STUDY AREA FOR THE ENTERPRISE MID - AMERICA PIPELINE WESTERN EXPANSION II PROJECT IN GARFIELD COUNTY, COLORADO WAS PROJECT # 11 -WAS -071 Submitted to the Board of County Commissioners Garfield County, Colorado By Robert Ficenec Stacy Goodrick Jana Pastor with contributions by Tracy Hall Colorado Bureau of Land Management Permit Number: C-39473 Western Archaeological Services 1600 Dewar Drive Rock Springs, WY 82901 March 14, 2012 ABSTRACT Enterprise Mid-America Pipeline (Enterprise MAPL) proposes to construct the Western Expansion Project II (WEP II) pipeline in eastern Utah and northwestern Colorado. The 95.47 mile long pipeline route closely parallels one or more existing pipelines for nearly 99% of its entire length. The proposed pipeline departs Thompson Station in Grand County, Utah, and proceeds northeasterly along the southern margin of the Interstate 70 corridor to Harley Dome, then parallels Highway 6/50 to a point 8 miles northwest of Mack, Colorado. The pipeline then continues northeasterly to West Salt Creek and follows Baxter Pass Road through the West Salt Creek canyon of Mesa and Garfield Counties to the former railroad town of Atchee. The pipeline continues northwesterly through Railroad Canyon, crossing Baxter Pass, and then follows Baxter Pass Road through the Evacuation Creek and West Evacuation Creek canyons of Garfield and Rio Blanco Counties, Colorado, and Uinta County, Utah, to where it ties into Dragon Station 1 mile north of the former mining town of Dragon, Utah. The study is for a linear ROW route of 24.66 miles, 1.59 miles of access road (14.27 linear acres on BLM and 16.23 linear acres on private), and 33.7 block areas (7.73 block acres on BLM and 25.97 block acres on private) in Garfield County. These are situated within the northern portion of the Colorado Plateau, and are located along West Salt Creek and West Evacuation Creek within the Book Cliffs -Roan Plateau regions. The project lies in Sections 5, 6, 8,16,17, 20, 21, 26, 27, 28, 33, 34, and 35, T5WS, R103W, Sections 13, 24, 25, 26, and 35, T6S, R104W, Sections 2, 3, 10, 11, 14, 23, 26, 27, and 34, T7S, R104W, and Sections 3, 9, 10, 15, and 16, T8S, R104W. This work was undertaken to ensure the project's compliance with county, state, and federal laws and regulations governing the identification and protection of cultural resources on privately owned lands that will be affected by a government action. This work was performed under BLM Permit No. C-39473. The purpose of the cultural resources investigation was to identify previously recorded resources within or near the project area that may be adversely affected by the proposed action as part of the Class I, to inventory the proposed pipeline route to a width of 200 feet (60m), to inventory the 14 TUAS and 10 Access Roads, and to evaluate those resources identified. Within Garfield County, a total of 603 acres (262.2 BLM and 340.8 private) was subject to an intensive (Class III) inventory. The Class I file search was conducted at the Grand Junction Field Office on May 13, May 16, and August 17, 2011, at the White River Field Office on August 2 and 3, 2011. The Class III inventory was conducted from June 14 and 16, and August 11 to September 1, 2011, with additional site recordation and view shed analysis conducted between September 8 and October 13, 2011. The report preparation was conducted between October 25, 2011 and January 27, 2012. As a result 97 sites have been previously recorded within a mile of the project area, with 23 previously recorded sites and 9 newly recorded sites documented by the intensive inventory. Accordingly, a determination of effect for the project is will be determined by the BLM pursuant to Section 106 of the National Historic Preservation Act (36 CFR 800). INTRODUCTION This inventory was undertaken to ensure the project's compliance with state and federal legislation governing the identification and protection of cultural resources on privately owned lands that will be affected by a government action. It was done to meet requirements of the National Historic Preservation Act (as amended in 1992), the National Environmental Policy Act of 1969 (42 U.S.C. 4321), the Federal Land Policy and Management Act of 1976 (43 U.S.C. 1701), and the Archaeological Resources Protection Act of 1979 (16 U.S.C. 470aa et seq., as amended), and Article 80.1, Colorado Revised Statutes. These laws are concerned with the identification, evaluation, and protection of fragile, non-renewable evidence of human activity, occupation, and endeavor reflected in districts, sites, structures, artifacts, objects, ruins, works of art, architecture, and natural features that were of importance in human events. Such resources tend to be localized and highly sensitive to disturbance. All work was performed according to guidelines set forth by the Office of Archaeology and Historic Preservation (OAHP) of the Colorado Historical Society. PROJECT LOCATION The proposed 95.47 mile long WEP II pipeline route departs Thompson Station in Grand County, Utah and proceeds northeasterly along the southern margin of the Interstate 70 corridor to Harley Dome, then parallels Highway 6/50 to a point 8 miles northwest of Mack, Colorado (Figure 1). The pipeline then continues northeasterly to West Salt Creek and follows Baxter Pass Road through the West Salt Creek canyon of Mesa and Garfield Counties to the former railroad town of Atchee. The pipeline continues northwesterly through Railroad Canyon, crossing Baxter Pass, and then follows Baxter Pass Road through the Evacuation Creek and West Evacuation Creek canyons of Garfield and Rio Blanco Counties, Colorado, and Uinta County, Utah, to where it ties into Dragon Station 1 mile north of the former mining town of Dragon, Utah. The route through Garfield County is depicted in (Figures 2-8). MODERN ENVIRONMENT The proposed WEP II Pipeline traverses a several environmental settings along its 95.47 mile long route, but is contained entirely within the northern portion of the Colorado Plateau physiographic unit. The Colorado Plateau, with its mountains, desert basins, and arid woodlands and grasslands, encompasses the southern Four Corners region of the Intermountain West (southeast Utah, southwest Colorado, northwest New Mexico, and northeast Arizona). It is located west of the Rocky Mountains in a region of generally flat lying sedimentary rock. Although the plateau has been bowed and buckled as a result of the collisions of continental plates that created the Sierra Nevada and Rocky Mountains, the sedimentary rocks remains relatively horizontal (Chronic and Williams 2002:293). The entire Colorado Plateau is located within the Colorado River drainage basin, with major rivers such as the Colorado, Little Colorado, San Juan, and Escalante rivers, as well as numerous smaller rivers and streams crossing the plateau. The numerous tributaries of the Colorado River have carved numerous steep sided canyons throughout the region. Folds and faults in many places have blocked the drainages, and have forced them to detour or cut through the hard underlying 2 Precambrian age rocks. Although the Plateau is an area characterized by relatively high elevations, the faults and folds have also resulted a wide range of elevations. The mean elevation on the Plateau is 1,936 meters (6,352 feet), but the elevational range of Plateau includes canyon bottoms at less than 750 meters (2,461 feet) and mountain peaks a staggering 3,840 meters (12,600 feet) above sea level. The Colorado Plateau is an arid to semi -arid region made largely up of deserts, with scattered areas of forests in the mountainous regions. In summer, the Plateau region receives limited moisture primarily as intense, local thunderstorms, with limited moisture arriving in the fall and winter as large frontal systems. The climate of most of the Colorado Plateau is classified as semi -arid, with total annual precipitation approximately 250 mm, with drier areas in the southern portion receiving as little as 130 mm, and higher elevations around the perimeter of the Plateau receiving as much as 670 mm (Hereford et al. 2002). Winters are cold, with moisture corning from the Gulf of Alaska and Pacific Ocean to the north and west. Summers are warm to hot, with a distinct wet period characterized by intermittent but often intense monsoonal storms coming from the eastern tropical Pacific, the Gulf of California, and the Gulf of Mexico (Adams and Comrie 1997, Barlow et al. 1998). Near Moab, Utah, in the heart of the Colorado Plateau, total average annual precipitation is approximately equal to the Great Basin desert to the north and the Chihuahuan and Sonoran deserts to the south. Both winter and summer precipitation are highly variable from year to year and has been linked to El Nino and La Nina patterns (Harrington et al. 1992, Hereford and Webb 1992, Cayan et al. 1999, Cook et al. 2007). La Nina is generally associated with dry winters, while El Nino usually leads to increased cool -season precipitation (Hereford et al. 2002). The Colorado Plateau is located primarily the Upper Sonoran and Transition life zones, but also has Canadian, Hudsonian, and Arctic -Alpine life zones at the highest elevations. In the subalpine regions of the tallest peaks, Engelmann spruce (Picea engelmannii) and subalpine fir (Abies lasiocarpa) are common. With decreasing elevation, these communities transition into a mixed -conifer forest with Douglas fir (Pseudotsuga menziesii), white fir (Abies concolor), Colorado blue spruce (Picea pungens), and ponderosa pine (Pinus ponderosa). Between 2100 and 1600 meters, pinyon/juniper woodlands dominate (Pinus edulis, Juniperus osteosperma, and on the southern edge of the Plateau, J. monosperma). The lower lying areas occupying most of the Colorado Plateau, is a mixed desert scrub community comprised of mostly low shrubs and perennial grasses. Sagebrush species (Artemisia tridentata, A. tridentata ssp. vaseyena, A. wyomingensis) are found at the higher ranges of the shrub land. At lower elevations, the dominant plants include blackbrush (Coleogyne ramosissima), Mormon tea (Ephedra viridis and E. torreyana), saltbush (Atriplex canescens, A. confertifolia and A. garrettii), and winterfat (Ceratoides lanata). The grass species of the Colorado Plateau include Indian ricegrass (Stipa hymenoides) and needle -and -thread grass (S. comata) and the Bouteloua gracilis, B. eriopoda, Sporobolus cryptandrus S. airoides, and galleta (Hilaria jamesii). Although the summer and winter precipitation amounts are similar, winter precipitation largely determines total annual primary productivity among perennials (Caldwell 1985). Winter precipitation accumulates in the soil due to the low evaporative demand and low transpiration rates at that time of the year. Plants begin to use these soil moisture reserves in early March, when plant growth is triggered by warmer temperatures. By late June, the driest month of the year, reserves of winter soil moisture near the soil surface are largely depleted and shallow -rooted perennial plants go dormant, whereas deeper -rooted plants take up residual water from deeper in the soil profile. Summer precipitation from late July to mid-September usually creates only limited soil moisture that can only be used by plant species with active, shallow root system such as the various grasses and late summer annuals. 3 Species of non -domesticated fauna of economic importance to both historic and prehistoric people in the Colorado Plateau. Bison evidently once occupied the project area (Burt and Grossenheider 1976), though probably in relatively low numbers (Meaney and Van Vuren 1993). Important Artiodactyla include elk, big horn sheep, mule deer, and pronghorn. Although pronghorn were probably most abundant in the open spaces of the Grand Valley of west -central Colorado, modern distributions may not accurately reflect their former range. Cottontail species occur in nearly all habitats, with jack rabbits and prairie dogs prevalent in open areas at lower elevations. Common predators included coyote, mountain lion, bobcat, black bear, and formerly grizzly bear, lynx, river otter, and wolf. Various rodents, reptiles, fish, and birds were also of economic importance, with numerous types abundant in the project area. For descriptive purposes, the portion of the pipeline located in northwestern Colorado is divided into two physiographic units, including the Mancos Shale Lowlands section, and the Books Cliff -Roan Plateau Section. Mancos Shale Lowlands Section The Mancos Shale Lowland section extends east of Utah's San Rafael Swell to the vicinity of Palisade, Colorado, following the base of the Book Cliffs (Horn et al. 1998d:8). Cretaceous -aged Mancos shale forms the bedrock in the central portion of the section. These soils were laid down over within the inland Mancos Sea. The Manco Sea advanced and retreated numerous times, laying down layers of salty soil which developed into the Mancos Shale formation which range to as much as 4,150 feet thick. The resulting clayey soils of the majority of the Grand Valley developed from these Mancos shale deposits. Alluvial soils occur along the intermittent streams that emanate in the Book Cliffs, and on the Roan Plateau, and flow southwards to the Colorado River. Alkaline soils are widely distributed, and as a result, desert shrubs such as shadscale, salt bush, and greasewood dominated the floral community. Scattered juniper, sagebrush expanses, and grasslands occur in the higher elevations at the base of the Book Cliffs. Elevations along the pipeline corridor in the Mancos Shale Lowlands generally range between 4400 ft (1341 meters) and 4900 ft (1493 meters). Because of its low elevation, the section is comparatively warm and dray. Climatic data from Fruita, Colorado, near the project pipeline indicate that mean maximum temperatures are 66.5° F, mean minimum temperature is 34° F. The Fruita area receives an average of 223 mm of precipitation per year, with approximately 38 cm of snow falling each year. Book Cliffs -Roan Plateau Section Just inside Colorado in the Grand Valley, the proposed WEP H Pipeline turns northward along West Salt Creek to cross the Book Cliffs -Roan Plateau. The Book Cliffs -Roan Plateau extend from the Mancos Shale Lowlands northward to the Uinta Basin and encompass the northern portion of the proposed pipeline. The Book Cliffs -Roan Plateau are largely composed of Cretaceous -aged sedimentary materials, with the uppermost layer consisting of the Mesa Verde Sandstone formation, which overlies the Mancos Shale formation. The deposits include buff to yellowish -brown sandstone bedded with soft gray shale that has one or more beds of bituminous coal, and underlying, thick beds of sandstone. The Book Cliffs -Roan Plateau is comprised of an uplifted syncline or structural depression, elevated approximately 3000 ft (914 meters) above the Grand Valley (Horn et al. 1998d:8). The south end of the section has been lifted the highest, forming a cuesta-like 4 feature that dips to the north. The ruggcd south side drops in two major cliffs. the higher Roan Cliffs. and the lower Book Cliffs. The north sloping plateau on top of the section is the Tavaputs Plateau. Elevations of the Tavaputs Plateau exceed 8000 ft (2438 meters), and in places 9000 ft (2743 meters). The proposed pipeline crosses Baxter Pass at an elevation of 8422 ft. The Book Cliffs -Roan Plateau section is drained to the south by the Colorado River and its tributaries. with the northern portion drained to the north and west by the White River. Because of the high elevation, surface water is relatively abundant, with numerous springs and permanent small creeks. At 8600ft, the annual precipitation is approximately 648 mrn, with much of the precipitation occurring in the form of snow. Snowfall may exceed 100 inches (Grady 1980). Vegetation in the section is closely tied to the elevation. Lower elevations support stands of pinyon pine and juniper, often with a sagebrush understory. Higher elevations support Gambel oak, service berry, and mountain mahogany, with aspen and pine forests located at the highest elevations. with a sagebrush or snow berry understory. PREVIOUS WORE AND CULTURE HISTORY Summary of Previous Work The file searches were conducted Robert Ficenec and Tracy Hall of WAS at the Grand Junction Field Office on May 13. May 16, and August 17. 201 I, and at the. White River Field Office on August 2 and 3, 2011. The base topographic maps at the BLM offices were examined to detennine which previous projects and previously documented sites were located within one mile of the project area, with the on-line database on COMPASS examined to provide additional survey and site information not available at the BLM field offices, Government Land Office Maps (GLOs) were examined to look for historic resources in the project area Several linear sites were noted and are discussed below. The data and literature review focused on identifying sites and cultural resource investigations that had been conducted within a 1 mile wide arca centered on the proposed WEP 11 pipeline route. This review identified 160 reports that have been done in the general area, which are listed in Table 1. The files search indicated 99 cultural resources occur within about one mile of the study area (Table 2). Culture History Prehistoric Period Advances in our knowledge of the prehistory of the northwestern Colorado and eastem Utah have come about through the systematic collection of data over a number of years. Academic and cultural resource management research has incrementally expanded our insight into prehistoric lifewuys and led to more focused research. The WAS research model begins with intra -site studies, focusing on the identification of specific activity areas within specific occupations. The next analytical level examines the use ofthe landscape. Since the advent ot'the "New Archaeology" in the 1960s. the dominant paradigm has stressed theinvestigation of behavioral and formational systems underlying the organization of the archaeological record (Willey and SablotT 1980:186; Dunne!! 1980:38). Topographic location, season of occupation. and function of activity areas all give insights into the aboriginal decision- making process and the organizational systems which are part of the larger settlement and 5 subsistence system. Additionally, studying diachronic changes provides data pertinent to technological innovation and cultural adaptation. Different site types have been defined that are ubiquitous across the landscape and are relatively unchanged through thousands of years. Examples of this pattern were found during the excavations of sites along the MAPCO Rocky Mountain Expansion Pipeline (Horn, Fetterman, and Honeycutt 2003). Sites 5GF620 and 5RB950 both revealed multiple cultural components dating from the Archaic to the Formative eras with evidence of short term hunting activities. Different adaptation strategies produce a variety of site types, such as residential camps of long or short duration, temporary camps, kill and/or processing sites, other extraction sites, and hunting stands. A major distinguishing characteristic between these site types was the duration of occupation and how the length of occupation affected the content and patterning of material remains. The study of intra -site variation was used as a means of building a framework to characterize regional patterns of land use. Identifying changes in regional patterns is critical to understanding the prehistoric utilization of the landscape through time. As Binford noted, "to reconstruct the entire pattern of land use, archaeologists have to be able first to identify the specific function of each separate site and then to fit all the individual parts together" (1983:131-132). Binford's (1980) observations showing that hunter -gatherers organize along a continuum of strategies between two extremes, foraging and collecting, have laid the groundwork for much debate in archaeology. This forager -collector model and others of a similar nature (e.g. Bettinger and Baumhoff 1982) provide the archaeologist with a powerful set of tools for interpreting archaeological remains. In addition to organizational and mobility models, approaches that measure energy costs have utility in the study of subsistence. Derived from optimal foraging theory, these models are used to assess the practicality of hypothesized subsistence strategies. When evidence of resource use in the archaeological record is encountered, archaeologists construct simple models of resource use. These models can then be tested and refined through the use of ideas drawn from diet breadth and other optimal foraging -based models. By assessing things like potential caloric yields and estimating time and transport costs, one can test the practicality of these resource -use models. Often, an assumption concerning the use of a certain resource or food will prove to be flawed once a practical measure of its utility is applied. The ordering of archaeological material into an accurate regional chronology is paramount to the understanding of prehistory in an area. Cultural complexes are defined mainly on the basis of artifact assemblages recovered in high -integrity components. Like most regions, early researchers in northwest Colorado and northeast Utah utilized the cultural chronologies from the more -studied surrounding areas but as the understanding of the archaeological records grows, chronologies have been refined. The northwest Colorado cultural chronology was originally defined by Reed and Metcalf (1999) and recently revised by the same authors (Metcalf and Reed 2010). Paleoindian Era The Paleoindian era is the oldest for which there is solid archaeological evidence. It begins at roughly 13,400 B.P. and ends around 8350 B.P. This is the transition period from the periglacial conditions of the Wisconsin ice advance during the terminal Pleistocene to the warmer and drier climatic conditions of the Holocene. Lush grasslands and savanna -like conditions predominated, with notably higher precipitation than today. This increased biomass supported a variety of large herbivore such as the mammoth, horse, camel, and extinct forms of bison. The lithic technology of the Paleoindian period is distinctive for its meticulous workmanship in the manufacture of projectile points. Projectile point styles are distinctive and serve as 6 chronological/cultural indicators within the period. Projectile points are usually lanceolate, some have distinct shoulders or stemmed, basally ground hafting elements, but they lack notching evident in the later periods. Paleoindian tool assemblages are characterized by a high percentage of gravers and spurred end-scrapers, and burination, especially on broken projectile point fragments (Frison 1978:77-78). More variation with the projectile point styles is seen after about 10,000 B.P., perhaps representing the presence of diversified cultural groups during the Pleistocene/Holocene transition. Much of the data from the Paleoindian period was initially derived from sites on the Northwestern Plains, most of which are specialized bison kills or sites associated with large game procurement. Preservation played a large role in the interpretation of the Paleoindian focus on large game. Perishable items do not stand the test of time like robust faunal elements. Also, large bone beds are much more visible resulting in their identification and investigation. However, as work progresses researchers are recognizing that early Americans had a wide and varied diet and generalized subsistence strategy, and a variety of plant and animal remains are being found in older sites (Kornfeld 2008). In the Great Basin, a far different picture of the early inhabitants has emerged. The term Paleoindian is not widely used, primarily because what little subsistence data are available suggest that these peoples were essentially broad-spectrum foragers who did not rely on Pleistocene megafuana and were more similar to foragers of the following Archaic period (Madsen 2007). The Paleoarchaic foragers were characterized by small, mobile foraging groups tethered to marsh ecosystems associated with terminal Pleistocene lakes. Pleistocene megafauna were not the primary focus but instead, they subsisted on fish, seeds, plants, and small mammals. Large mammals were comprised of antelope and species commonly found in Archaic assemblages. In the study area, the Paleoindian era is represented by four traditions that can be distinguished largely on the basis of projectile point styles. These traditions include the Clovis, Goshen, Folsom, and Foothill/Mountain. Projectile point characteristic of the Clovis tradition are large, fluted, finely-made lanceolate points. Clovis points have been found in association with extinct megafauna. Although Pleistocene megafauna remains have been identified in northwest Colorado or northeast Utah, no Clovis artifacts have been found with these remains (Schroedl 1991). The Goshen tradition has been a controversial concept until recently, and was first thought to be a variant of Clovis. Excavation at the Mill Iron site (Frison 1978) eliminated much of the uncertainty of Goshen's relationship with Clovis and Folsom. Many Goshen points bear a strong resemblance to the Plainview type as it is known from the Southern Plains. The points are basally thinned and not fluted. The Goshen tradition dates between 12,950 and 12,650 B.P. Folsom projectile points are widespread on the Plains and in the Rockies. Folsom projectile points are finely made with the highest quality pressure flaking techniques. The specimens can be fluted or unfluted. An extensive Folsom assemblage (10,500 B.P.) was found at the Barger Gulch Locality B in Middle Park (Korneld et al. 2010). The assemblages included broken finished and exhausted projectile points, scrapers, gravers, ultrathin bifaces, Levallois-like cores, concentrations of burned specimens suggesting hearth locations, several types of activity areas, and dwellings. The Foothill-Mountain tradition favored more hunting and gathering subsistence in foothill and mountain slope areas and were more Archaic in terms of subsistence strategies (Kornfeld et al. 2010). These people procured deer, bighorn sheep, and pronghorn as well as exploiting floral resources. The projectile points are unfluted and exhibit a lanceolate shape with restricted stems and indented bases. Kornfeld et al. (2010) argue that there is now sufficient data to support the concept of a dichotomy in subsistence strategies between plains and foothill-mountains ecosystems that varied in intensity throughout prehistoric times. In Pitblado's study of Paleoindian projectile points 7 from western Colorado, she notes that there is extensive evidence of the Foothill -Mountain tradition (Pitblado 1994). She argues that the generalist subsistence practices indicate a closer cultural affinity with Great Basin Paleoindian groups. Site 42GR1547 is located along the currently proposed WEPII pipeline. The site was subjected to data recovery excavations during the MAPCO, Rocky Mountain Expansion Project (Horn, Fetterman, and Honeycutt 2003). The site dates to between 9550 and 9270 B.P. Surface artifacts included Elko Eared and McKean Lanceolate projectile points. Cultural material recovered during excavation was sparse and included debitage, scraping tools, and gravers. Site interpretations were limited because of the paucity of cultural remains, however, paleoenvironmental studies revealed a cool, dry environment, with mesic species. Cottonwood Creek was flowing water within a riparian environment. The Cisco Desert is now an arid shrubland with sparse vegetation. Site data suggests that cultural manifestations are similar to those found in the northern Colorado Plateau. Research questions for the Paleoindian era are plentiful because of the paucity of investigated sites dating to this time period. The Clovis and Goshen traditions are still largely enigmatic because the site sample is so low. The boundary between the Foothill -Mountain tradition and the following Archaic era is becoming more and more blurred as it appears that an "Archaic" lifestyle was practiced much earlier than previously thought. Paleoenvironmental changes have been suggested by previous excavations at Site 42GR1547. More information is needed to fully understand the environmental conditions present during this time period. Interrelationships between the Colorado Plateau, Plains, and Great Basin groups needs further study as well. Any sites with even minimal information would be of importance to our understanding of this era. Archaic Era During the Archaic era there was more intensive utilization of plant foods and exploitation of a broader range of fauna than in the preceding Paleoindian era. The Archaic is recognized as reflective of highly mobile groups who left an overlapping labyrinth of cultural remains on the landscape. There is a great deal of cultural continuity during this time span with a series of cultural changes. The high mobility was a defining factor in subsistence -settlement practices. Small groups of a single family or extended family moved as resources became available. Their intimate knowledge of resource patches, seasonality, and availability dictated their deliberate movements across the landscape. This logistical system included brief stops in some areas and more extended stays in others depending on resource availability. Reed and Metcalf (1999) defined four "periods" within the Archaic era based on changes in adaptive strategies through time. These included the Pioneer period, characterized by the establishment of full-time seasonally scheduled settlement systems in all of the major basins; the Settled period which saw a fluorescence of locally oriented populations within a central -place foraging strategy centered on predictable winter habitation areas; the Transitional period, characterized by increasing variability in settlement patterns and less sedentary habitations; and the Terminal period which featured early experimentation with various forms of resource intensification to cope with apparent stress in settlement systems (Reed and Metcalf 1999:79). The utility of the archaeological units proposed by Reed and Metcalf in 1999 has been questioned and in 2010 Metcalf chose to drop the periods in favor of the terms Paleo-Archaic, Middle Archaic, and Late Archaic. In the Class I overview of the Grand Junction Field Office, the Archaic was divided into four periods referred to as Paleo-Archaic, Early, Middle and Late by Berry (2011). As work progresses and more data becomes available, the utility of sub -dividing the era (e.g. 8 Metcalf 2010 and Berry 2011) or following the Stiger (2001) example of viewing the Archaic as an overall period without use of sub -divisions, will continue to be examined and refined. The Metcalf and Reed (2010) revision lists six adaptive periods with associated trait lists. Interwoven in the adaptive periods are "anomalies" which represent disruptions to the stable adaptive pattern. The trait list is meant to be an indicator of the data available at the present time. The earliest adaptive period (Adaptive Period 1) occurs between 9000-9500 B.P. Diagnostic artifacts are few, with the exception of Deception Creek points. The climate is cool and moist and faunal material includes medium artiodactyls and small mammals. There appears to be high mobility and simple basin hearths are utilized. Adaptive Period 2 is characterized by the appearance of the first house pits, roasting pits, and Elko Corner -notched projectile points. The period falls between 8400 and 7900 B.P. and the climate is warmer and drier than the previous period. Small mammals are dominant with evidence of ground stone use for plant processing. Adaptive Period 3 begins at 7200 and ends at 5800 B.P. The xeric conditions during this period led to the aggradation of sediment. House pits are utilized and the faunal remains are dominated by medium artiodactyls. Elk, Northern and Narrow Series side -notched points appear early in this period. There appears to be more sedentism with longer duration occupations. Adaptive Period 4 ranges from 5200 to 3900 B.P. It appears that house pit use had ceased as a consistent pattern by about 4900 B.P. (Metcalf 2010:31). McKean style projectile points appear at about 5000 B.P. The climate experienced a change to cooler than today and the "Spring Creek paleosol" develops. Metcalf (2010) suggests that during the coolest part of this interval the area became too cold to continuously support winter occupations, but at the same time the relatively more mesic conditions supported higher game populations and the seasonal emphasis may have become warm season oriented. The neoglacial cooling would have also affected medium artiodactyl populations and rabbits likely would have gained importance. By Adaptive Period 5 (3600-2500 B.P.), house pits no longer appear in the archaeological record. There appears to be an increase of large artiodactyls in the faunal record. Ground stone declines in the later part of the period and projectile points demonstrate great diversity. The period starts with a warmer interval and then experiences neoglacial cooling (Metcalf 2010). Adaptive Period 6 is the last interval in the Archaic era and dates between 2200-1800 B.P. Rabbits increase in importance and there is some evidence of rodent use. Roasting pits decline and there is a lack of ground stone. The climate continues to be cool. As in the Wyoming Basin, there are two areas of research that are very intriguing during the Archaic era. These research areas include the presence and use of house pits and the presence of "McKean" style projectile points. House Pits There is a decided lack of house pits between 4800-4100 and 3600-2500 B.P. and in Colorado Plateau. Because the distribution of house pits is highly patterned temporally, Metcalf postulates that they reflect a subsistence and mobility pattern that is archaeological distinctive and appears when conditions make it an effective solution (Metcalf 2010:19). As in the Wyoming Basin, the perception of the distribution of house pits may change as additional houses are discovered. Cold weather environments require some protection from the elements (Gilman 1987) and it stands to reason that some sort of structure was used throughout the prehistory of the Colorado Plateau. The remains of different types of structures may not leave an archaeological signature or environmental conditions operating at certain times may have obscured the evidence. There are a large number of 9 unresolved questions about prehistoric house pits including aspects of construction, use, maintenance, season of occupation, duration of occupation, variability of house types, identification of house pits, the role of storage, and implications for mobility, and other questions that remain important in house pit studies. A cultural component at Site 42GR1548 (Cisco Inferno) contained a small house pit structure with post holes that dated to between 2660 and 2500 B.P. The abundance of greasewood charcoal indicated a superstructure of greasewood. The small size of the house pit indicated a spring, summer, or fall use. A similar house pit site is located to the east of 42GR1548 near the state line. Site 5GF126 is slightly larger and contained post holes (Horn, Fetterman, and Honeycutt, 2003). House pits dating to any time period with good integrity will result in data recovery. McKean The McKean Complex on the Northwestern Plains first occurred during the Middle Archaic and is characterized by a shift in subsistence patterns as compared to the preceding Early Plain Archaic period. The bison -oriented subsistence strategy also includes a shift towards an increased reliance on gathering and processing plant foods as compared to earlier periods. (Kornfeld and Todd 1985; Frison 1991). The complex is defined by McKean Lanceolate, Duncan, Hanna, and Mallory projectile points (Kornfeld et al. 2010). These style points are widespread across the Wyoming Basin and Colorado Plateau, as well as the Northwest Plains. The McKean complex appears to have developed into a well-established endemic cultural tradition in the Big Horn Basin, whereas in southwest Wyoming and northwest Colorado the appearance of these projectile point styles is problematic. The underlying question is, did these point styles appear in the context of an adaptation by local Archaic groups or did McKean groups occasionally occupy the Colorado Plateau during the Middle Archaic, much like McNees (2005) postulates for southwest Wyoming? Schriever (2010) accurately notes that the only unifying aspect of the McKean Complex is the point style, and possibly the observation that most sites with McKean material are camps interpreted as broad-spectrum forager sites. Very little comprehensive analyses have been completed on McKean components which makes any assumptions premature. Metcalf (2010) poses five research questions which include: Is the McKean Complex a useful construct for describing the Middle Archaic in northwestern Colorado? Are there any data to support the idea that there is a temporal sequence for the introduction of the individual McKean point types (Lanceolate, Duncan, and Hanna)? Is there a correlation between the occurrence of McKean points and the hunting of big game? Does the presence of reliable populations of bison correlate with McKean distributions? Does the presence of McKean points indicate a relatively mobile hunting -focused economy? Metcalf concludes by stating that although the McKean Complex remains a useful construct for discussion of the Middle Archaic, at this time there is simply not enough data to determine the cultural dynamics at play during this time period. A McKean style projectile point was found on the surface at Site 42GR1547. Further studies of cultural components containing McKean style projectile points are needed. 10 Archaic Settlement and Subsistence At a general level, the forager/collector spectrum provides a model with which to compare the settlement and subsistence patterns during the Archaic era. But it can be assumed that placement on the spectrum would vary through space, time, and probably season for even the same cultural group. At certain times we would expect foraging for a wide range of roots, seeds, greens, small game and occasional large game. At other times a logistical orientation targeting large game and specific resources would have been used. It must be recognized that the subsistence strategy being practiced at any time was fluid, responding to a number of cultural and natural variables. Nonetheless, there are broad patterns in settlement and subsistence that can be elucidated in the archaeological record. The detailed settlement -subsistence model described in an earlier section presents a working model of a general Archaic -Late Prehistoric annual round. This model needs refinement for particular periods and locations in the region. The inability to identify indicators of seasonality in the archaeological record is a major impediment to understanding prehistoric settlement, subsistence, sedentism, and mobility. Archaeofaunal data provide good potential for seasonality information based on seasonal increments in animal tissues plus ages of animals born in discrete seasons. These can be measured with tooth eruption and wear, bone metrics, bone epiphyseal fusion, dental cementum increment analysis, and other methods. The presence of seasonally -limited plant remains has also proven useful. The potential effect of storage for future consumption can obfuscate the meaning of seasonality data, and this is an area in need of investigation. Although settlement -subsistence evidence is limited for the Archaic era, it exhibits variability in the spatial and temporal distribution of different types of cultural remains, guided by environmental conditions. Environmental conditions ranging from the dry, hot Altithermal to the wetter, moister Neoglacial affected both floral and faunal communities, with obvious impacts on the human population. Sites dating to any age containing evidence of seasonality are important to our understanding of the settlements -subsistence patterns at work during the prehistoric period of the Colorado Plateau. Topics of interest also include: a) species identification; b) study of extractive technology; c) estimation of mobility patterns; d) settlement analysis; and e) synchronic and diachronic comparisons. Specific questions include how evolutionary ecology models and Binford's (1980) model of hunter/gatherer organizational systems can be applied to settlement and subsistence evidence from sites in the project area, across the range of functions and ages that are likely to become evident. Early Archaic sites dating from 9500 B.P. and 4700 B.P. are relatively rare and thus good candidates for data recovery. Our knowledge of the transition from the Paleoindian to the Archaic era is limited and the changes in subsistence and settlement patterns need to be further defined. The later part of the Archaic era is not as well represented in the Colorado Plateau as in the Green River Basin to the north but there is more information available than during the early part of the era. Sites with high quality spatial integrity would be candidates for data recovery. Formative Era The Formative era in the region originally extended from 2350 B.P. to 650 B.P. (Reed and Metcalf 1999:98) and refers to the period when corn was a major subsistence focus in some portions of western Colorado (Jett 1991; Stiger and Larson 1992). However, farming is not a necessary trait for inclusion into the Formative era in the Colorado Plateau. The higher elevations were limited in their agricultural potential due to their short growing season, and other areas lacked the water and 11 soils required for viable horticulture. Consequently, horticulture, sedentism, and mobile hunting and gathering occurred contemporaneously, often separated only by elevation or precipitation barriers. Substantial habitation structures and pottery becomes common with the more sedentary groups. Reed (2010a:20) proposes the term as an "archaeological unit as reference for sites contemporaneous with farming adaptations". The Formative Era is broken down into the Gateway, Aspen, Anasazi, and Fremont traditions and includes the introduction of the bow-and-arrow, habitation structures, ceramics, and horticulture and is characterized by a spike in radiocarbon data. The Anasazi Tradition (1100-900 B.P.) is usually found toward the southern portion of the Northern Colorado River Basin where irrigation agriculture was viable. Anasazi groups relied heavily on corn beans, squash, and several other cultigens, and produced high-quality ceramics. Anasazi sites are distinguished by substantial rock structures, pottery, and rock art styles. No Anasazi sites exhibiting typical habitation structures have been documented in the project area. However, rock art sites attributed to the Anasazi and Anasazi-style ceramics have been noted in the general area (Cole 1987; Reed and Metcalf 1999:98) These have been attributed to Anasazi forays into the area or to trade and/or influence of Anasazi culture on other peoples. In general, there does not appear to be a bona fide Anasazi occupation in northwestern Colorado. Farther to the south and southwest of the project area are the Northern San Juan Anasazi. The Gateway Tradition (2350-750 B.P.) is a generalized horticultural tradition reflecting local adaptations with limited reliance on corn, beans, and squash in the interior basins and foothills where soil, moisture and growing seasons were adequate. Pottery was manufactured, but was also traded for with adjacent Anasazi and Fremont groups. Masonry surface structures were built, and granaries and storage cists often occur in rock shelters. Gateway Tradition rock art was influenced by Anasazi and Fremont styles. The tradition saw the introduction of the bow and arrow during the early part of the period, which used the small, corner-notched projectile points of the Rosegate series. The 1984 context for west-central Colorado suggests that Formative-groups were best classified as distinct from either Fremont or Anazazi traditions. Reed (1997) agreed with the idea that there are enough distinct qualities to justify separation and posited the Gateway tradition. Others like McMahon (1997), believe that most of those sites could and should be regarded as Fremont. Gateway tradition sites with substantial masonry architecture, evidence of corn, small quantities of Anasazi ceramics, and that date to between approximately 2350-750 B.P. do not appear to have a very useful application in the project area. The Gateway Tradition is a recent archaeological unit and, as the database of sites continues to grow in the region, it may be useful to further differentiate the various cultural resources in the area. The Fremont Tradition (800-600 B.P.) is also characterized by substantial structures, high- quality ceramics, and a reliance on corn, beans, and squash agriculture. It is found in the western portion of the Northern Colorado River Basin at the lower elevations where soils, moisture, and growing seasons are adequate. It is distinguished from the Anasazi by distinctive structure, pottery, basketry, and rock art styles. To the northwest of the project area in the Uinta Basin of northeastern Utah and northwestern Colorado, the Uinta Fremont have been identified and may contain sub-regional variants such as the Douglas Creek/Dinosaur group(s), and the Tavaputs Plateau group(s). To the west of the project area in Utah, the San Rafael Fremont have been identified. Evidence of the Fremont tradition has been noted in the western Colorado Plateau and "approximately 300 sites recorded in western Moffat and Rio Blanco counties have been attributed to the Fremont tradition" (Reed and Metcalf 1999:113). Site types include rock art, open and sheltered artifact scatters, and architectural sites (mainly granaries) (Gardner et al. 2005a, 2005b). The region is adjacent to major concentrations of Fremont 12 culture in lower elevation areas to the west, particularly in nearby Douglas Creek (Creasman 1981), and more distant areas such as Dinosaur National Monument and the Uinta Basin along the Green River in Utah (Jennings 1974). However, some controversy exists concerning Fremont occupations in the area. Basin houses attributed to the Fremont tradition have been noted, but are not as common as houses from the same time period further to the north in Wyoming. Settlement and subsistence data may suggest more short-term patterns with low quantities of sites with ceramics and the absence of aggregated settlements. It has been suggested that Fremont practices in the area merely represent a continuation of the in situ Archaic practices with limited horticulture as a relatively insignificant addition to the lifeway (Reed and Metcalf 1999). However, recent work at the Eagle Point rock shelter (5RB4662) and Kuck rock shelter (Gardner et al. 2004, 2007, 2008a, 2008b) may support Grady's (1980) proposed Fremont occupation in the Piceance Basin. In addition, Gardner (2009:130) states that the Douglas Creek area contains a high accumulation of agriculture sites and numerous permanent signs of agriculture that support a degree of Fremont commitment to the landscape. The Aspen Tradition (2350-700 B.P.) is specific to the Northern Colorado River Basin where horticulture was not possible due to the short growing season. Consequently, a generalized hunting and gathering subsistence pattern was employed which focused on deer, pronghorn antelope, elk, and bighorn sheep. Bison were taken when available. Associated pottery is usually ascribed to the Anasazi or Fremont traditions, but generic gray -wares were also manufactured. The bow and arrow was introduced during the early part of the period, using a wide variety of small, corner- and side - notched projectile points. Also characteristic of the tradition are slab -lined and rock -filled roasting pits, ground stone, the procurement of small game such as rabbits and rodents, and the gathering of seeds, roots/tubes, and other edible plants. This tradition was proposed because many of the sites in the area attributed to the Fremont tradition lack artifacts diagnostic to that tradition (Reed and Metcalf 1999). No evidence of permanent Fremont farming settlements has been noted in the region and the Aspen tradition is based on what is lacking in the archaeological record rather than by what is present. Like some of the original concepts regarding this area (Jennings 1976), the Aspen tradition represents local, non - Fremont populations that display Archaic -style hunter -gatherer adaptations and may have traded for corn and other Fremont -style artifacts. Others, such as Grady (1980) and Gardner (2009) posit that the area was used seasonally by Fremont peoples who farmed at lower elevation and used the upper elevations for hunting and gathering. Gardner (2009:134) goes on to state that the "Fremont used their agriculture fields in combination with other permanent tethers to indicate a level of propriety over specific space", and that " agricultural practices allowed the Fremont to continue a mobile lifeway". Formative era sites where there is no evidence for the practice of horticulture are numerous in the project area. However, problems arise in how to differentiate the hunting and gathering activities of the horticultural groups from those same types of activities being practiced by non - horticultural groups still following a more traditional hunter -gatherer lifestyle. Since both groups are known to use the same projectile points styles (Rosegate), may use generic gray ware ceramics or fire pits with rock filled basins, and are probably utilizing overlapping extended ranges for hunting and gathering, differentiation in terms of surface identification based upon survey data is difficult. In southern Wyoming, the Uinta phase (Thompson and Pastor 1995) is commonly applied to components that largely coincide with the Formative era and exhibit many of the same characteristics of Aspen tradition sites. It may be useful to maintain the Uinta phase so that Formative -era components in the region can be contrasted to Aspen tradition sites (Reed 2010a). 13 The Formative era encompasses a wide range of behaviors, adaptations, and archaeological evidence. Further research will help to better define the utility of the archaeological units and refine the chronology in the area. As the known site pool increases, refinements of the models of technology, subsistence, and settlement patterns will result. Protohistoric Era The Protohistoric period begins around 650 B.P. (A.D. 1300) with the collapse of the agricultural Fremont, and ends in A.D. 1881 with the expulsion of the Ute Indians to reservations (Reed and Metcalf 1999:146). It encompasses the period prior to European contact, through early settlement of the Southwest by the Spanish, to Euroamerican settlement and early statehood. The early, pedestrian, Protohistoric inhabitants were mobile hunters and gathers who continued an Archaic life -way. Acquisition of the horse after A.D. 1650 increased group mobility, cultural contact with other groups, and warfare. Late Protohistoric sites often contain small quantities of Euroamerican artifacts obtained in trade. Historic records indicate that the Ute and the Shoshone were the primary occupants of eastern Utah and northwestern Colorado during this time (Reed 1994). The Ute and Shoshone peoples share the Numic language as well as many elements of material culture. Historic accounts of Ute and Shoshone distributions indicate a boundary somewhere north of the Yampa River (Callaway et al. 1986; Gradyl984). Archaeological data provides limited support for Shoshone occupation of the project area. Protohistoric sites generally resemble Archaic sites and generally reflect similar subsistence, technology, and settlement adaptations. Diagnostic artifacts include Desert Side -notched and Cottonwood Triangular projectile points, and often Uncompahgre Brown Ware ceramics. Wickiups are sometimes associated with Protohistoric sites, however, they are perishable by nature and are likely under -represented in the archaeological record. Teepees were likely used more often after the introduction of the horse and stone circles are the primary evidence in the archaeological records. Reed and Metcalf (1999) present a two-phase construct based on Ute occupations with the Canalla phase extending from A.D. 1100 and when Uncompahgre Brown Ware appears in the region, and the Antero phase which represents a shift to a fully equestrian lifestyle and the appearance of Euroamerican trade goods. Alternate models for the Ute occupation of the area are based on historical models of phases of Native American history, beginning with the late pre -contact period and ending with a phase which describes the modern period (Baker et al. 2007; Leacock 1971). Reed (2010b) has slightly amended the construct of the Protohistoric era in northwest Colorado Plateau. The period between 650 and 550 B.P. is characterized by sites attributable to both the Fremont tradition and Protohistoric -era groups and may require an additional archaeological unit (Metcalf and Reed 2010:20). Radiocarbon data suggests that a transition from Fremont/Aspen tradition to Numic sites occurred around this time period and interaction and relations between the two groups may be visible in the archaeological record. The Protohistoric era in southern Wyoming is represented by three archaeological units (Thompson and Pastor 1995). The Firehole phase (650-250 B.P.), the Protohistoric period (250-150 B.P.), and portions of the Historic period (150 B.P. to the removal of Native Americans to reservations) overlap chronologically with the Protohistoric era in Colorado. The Wyoming model makes little to no cultural assumptions unlike the Reed and Metcalf (1999) Canalla and Antero phases which are intended to delineate changes in Ute culture. Dendrochronological dating of wickiup poles and radiocarbon dating of hearth fuel woods have generally provided the basis for chronological interpretations over the past few decades. However, biases such as the "old wood problem" may have ramifications for both the 14 dendrochronological and traditional radiocarbon dates for this period and other dating methods (AMS, thermoluminescence dating of ceramics, trade goods, etc.) may provide for more accurate data. Another chronological issue noted for Protohistoric -era components is the notable drop in radiocarbon dates between approximately 300 and 275 B.P. (Reed and Metcalf 1999; Reed 2010b). The paucity of dates may be attributable to sampling bias, however, Protohistoric sites are no less visible than Formative sites, so the drop likely represents a decrease in population. It has been speculated that it may represent a period of depopulation of the region because of the introduction of European diseases (Reed and Metcalf 1999; Reed and Smith Gebauer 2004). Protohistoric sites are sparsely and unevenly distributed in the area and overwhelmingly represented by field camps. This suggests greater mobility during the Protohistoric era than during the preceding periods. In addition, the subsistence model indicates that Protohistoric -era subsistence practices were much more like those of Archaic groups than they were like regional Formative -era groups. A focus on a narrower range of plant and animal foods, as well as more highly ranked animal foods is suggested (Reed 2010b). The Protohistoric era is characterized by less variability in projectile point types than any other archaeological unit with Desert Side -notched points and Cottonwood Triangular points dominating the assemblage. Ceramics and groundstone are rare and identified thermal features suggest a less focused approach to specialized cooking and shorter site occupation than in previous eras. The presence of Euroamerican trade goods, along with obsidian, marine and freshwater shell, and gilsonite in Protohistoric contexts suggest relatively elaborate exchange systems and increased mobility. The pool of Protohistoric -era components is relatively small and data gaps are plentiful. As with most models, the Protohistoric era should be continually reevaluated as additional excavation data from sites in the region are acquired. Historic Period Early Exploration The historic period began in southern Colorado with the early Spanish explorations of the late seventeenth century, and later, with trade between the Spanish and the native Ute Indians (Husband 1984; Mehls 1984). It overlaps with the Antero Phase (A.D. 1650-1881) of the Protohistoric -Historic Era defined by Reed and Metcalf (1999), and reflects regular contact with the Spanish from the south, increasing contact with Americans from the north, introduction of the horse, gun, and other trade goods, the expansion of the Rocky Mountain fur trade, and the consequent disruption and destruction of traditional lifeways. Archaeological historic ethnic affiliations in relation to modern Indian groups can be assigned with moderate certainty, primarily Ute, but possibly Shoshone in the northern portion of the study region. The Dominguez-Escalante Expedition of 1776 is often labeled as the first exploration of the Great Basin. It was intended to find a passable route between Santa Fe and Monterey, California. With the knowledge acquired by the previous Rivera expeditions the party was able to easily make their way into southwestern Colorado following the route of what would later become the Spanish Trail. They followed the Dolores River northward where it crossed the Uncompahgre Plateau into the Uncompahgre Valley and continued northward across the Colorado River to Rangely, then westward into Utah. Once in Utah, they cut their journey short and returned to New Mexico through the canyons of southeastern Utah and the Hopi mesas of northern Arizona. Part of the route used 15 by the expedition became known as the Old Spanish Trail and was used later by American trappers and traders. Fur Trade Early trappers occupied the region after 1800 and, after the region opened due to Mexican independence, the fur trade flourished from the 1820s to the 1840s. Antoine Robidoux established various trading posts in the area and Browns Park, located in northwestern Colorado, became a focus of the fur trade with the establishment of Fort Davy Crockett in 1836 (Husband 1984). Federal Exploration Federal exploration of the area did not begin in earnest until the 1850s. A large focus of the exploration was to locate transportation routes, especially a path for a transcontinental railroad. Several explorers led parties of expedition and survey through Colorado and Utah, and after the Civil War, several expeditions surveyed and mapped the area. John C. Fremont led expeditions that crossed northeast Utah and northwest Colorado. The Gunnison and Macomb expeditions subsequently crossed the region. These expeditions provided ethnographic, natural, and surveying information that eventually opened up the region to settlers. Mormon Settlement In 1855 the Mormon church established a mission in the Elk Mountains (now the La Sal Mountains) at the edge of modern-day Moab. The mission was summarily abandoned in the same year due to numerous attacks by both the Paiutes and Utes. The Mormons later returned to the Elk Mountain mission and founded the settlement of Moab in 1876. In 1861 Brigham Young sent a small party to explore the Uintah Basin for possible settlement. They reported that the area was barren and had no value so Young decided not to send settlers there (Fuller 2008). After the area was irrigated in the 1890s, Mormons and other farmers settled into the area. Reservation Era On May 5, 1864, Congress passed a law confirming President Lincoln's 1861 executive order and set up the Uintah reservation (Burton 1996). The Ute people were to give up their land and move within one year to the Uintah Reservation without compensation for loss of land and independence. The Uinta-ats (later called Tavaputs), PahVant, Tumpanawach, and some Cumumba and Sheberetch of Utah were gathered together at the Uintah agency during the late 1860s and early 1870s to form the Uintah Band (Burton 1996). The White River Utes were also forced to move to the Uintah Reservation in 1880. And finally, the Uncompahgre Utes were forced to relocate to the Ouray Reservation, adjacent to the southern boundary of the Uintah Reservation. Fort Thornburgh was built along the Green River in 1881 to maintain peace between settlers and to ensure that the Uncompahgre and White River Utes remained on the reservations (Burton 1996). Mining The late 1860s saw the development of the Hahns Peak and other mineral mining districts in Colorado (Athearn 1982). In 1888, Gilsonite was discovered in various parts of Uintah County and on the eastern portion of the Uncompahgre and Uintah reservations. Miners quickly persuaded the federal government to withdraw 7000 acres from the Uintah Reservation so that they could legally mine Gilsonite (Fuller 2008). Gilsonite added to the freight business between Price and Myton but the wagons could not keep up with the demand and in 1904 the Uintah Railway built a 16 narrow gauge line from Dragon, Utah to Mack, Colorado. Known for its sharp curves and steep grade, the railroad was shut down in 1939 because it became much cheaper to transport the Gilsonite by truck. The Price-Myton route continued to be used as a mail and stage line, however, this lasted only two years until a route between Vernal and Colton was established (Burton 1996). Coal was discovered in northwestern Colorado in 1890 near the town of Coalmont and limited mining activities occurred into the 1920s (Husband 1984) in places such as Carbonera (5GF1562). Farming and Ranching Beginning in the 1870s, the open range livestock industry moved into the region, but was eclipsed during the 1890s by smaller ranchers, and by the 1920s, the better lands had been homesteaded and most of the present communities had been established. The first cattle arrived in the late 1860s in northwestern Colorado and sheep were first brought to Uintah County in 1879 by Robert Bodily (Burton 1996) and constant conflict between sheepmen and cattlemen occurred during this time on the plateau (Husband 1984). Farming began in the area as soon the Utes were removed. Fruit dominated the Grand Valley and other crops like potatoes were grown and sold to mining camps (Husband 1984:79). In northwestern Colorado and eastern Utah, it was too high, arid, and cold for farming and the area became known for cattle and hay. Irrigation projects were essential for growth of these industries and various projects ranging from large Federal projects like the Grand Valley Project to small and isolated ranching and farming irrigation ditches were built from the 1880s through the mid 1900s. Transportation Local and regional roads were developed to service the mining and ranching communities. Toll roads were built around Grand Junction in the 1880s while smaller communities in the northwest were interconnected with stage and freight routes. Automobile transportation resulted in the construction of numerous road through the region. The Midland Trail, also called the Roosevelt Midland Trail, was a national auto trail spanning the United States from Washington, D.C. west to Los Angeles, California and San Francisco, California and was organized in 1912 by residents of Grand Junction, Colorado. From Denver, the original routing split several ways to cross the Rockies via Berthoud Pass, Tennessee Pass, Cochetopa Pass, and Monarch Pass. All routings converged in Grand Junction, Colorado and continued into Utah through Green River, Utah and Salt Lake City. Highway 6 and 50 was built in 1934, and roughly corresponds to the present-day route of Interstate 70. The forerunner of Highway 6 and 50 was the Pike's Peak Ocean to Ocean Highway. It also roughly conformed to the route used by Highway 6 and 50 but utilized the abandoned Denver and Rio Grand Railroad (D & RG) narrow gauge in Utah as it neared the Colorado state line. The western slope was opened further in 1882 when the D & RG reached Grand Junction and, in 1932, when D & RG completed the route through northwestern Colorado from Denver to Salt Lake City. In 1883, track laying for the transcontinental railroad was completed near Green River, Utah. Because the Denver & Rio Grande Western Railway constructed their major shops in Grand Junction, the population of the town grew tremendously. This line, the Alkali Division, ran between the town of Grand Junction and Green River, Utah. In 1889, the gauge was switched to the standard gauge and the line moved south of the Colorado River. The Uintah Railroad was operational from 1904 to 1939. The railway was founded in1902 as a subsidiary of Gilson Asphaltum Co. It linked the newly founded townsite of Mack with the mines in Dragon, Utah. The Uintah Railroad was well known for having some of the steepest and sharpest grades of any in the U.S. Over Baxter Pass, an 8437 foot mountain divide, the engines 17 climbed more than 2000 feet in six miles, featured 65 degree curves and a7.5% grade requiring a unique articulated engine to manage the line. Between Mack and Baxter Pass, 37 bridges were crossed. Atchee (5GF642.2) was located at the base of Baxter Pass; it was the location for the mechanic and repair shops. Sites which would be expected on the lines include sidings, depots, construction camps, grades, and charcoal lenses. Oil and Gas Since about 1900, oil and gas development has increasingly influenced the landscape of eastern Utah and western Colorado. Early exploration was widespread in the area with both oil and gas creating numerous mini -booms throughout the years. Oil shale speculation was at a high around 1915 and the government created the Naval Oil Shale Reserves in the Piceance Basin. The Historical Context for Colorado (Clark and Corbett 2007) provides a broad context and theme of oil and gas sites in Colorado. It briefly outlines periods of significance of oil and gas industry sites in Colorado ranging from 1860 to 1900, 1900 through the1930's, to sites post-dating World War II. Because of the variability of historical archaeological sites and the multitude of approaches that may be used in their research, identification of data gaps and what is most important at historical archaeological sites is a moving target. For the most current view regarding theoretical and research orientations, see the Colorado historical archaeology context (Church et al. 2007). In the project area, the historic sites of Carbonera (48GF1562), Dragon(48UN1802)and the Stanfield homestead (48GF 1561) have been previously excavated. Further research into these sites and site types including trails and roads, early settlements, farming and ranching, irrigation, mining, railroads, and oil and gas may fill data gaps and provide important information about the history of the area. PROJECT OBJECTIVES The primary objective of the Class III archaeological inventory was to locate significant cultural resources in the project area to aid in the preservation of these cultural resources or to facilitate the formation of appropriate mitigative strategies. A research design intended to guide all field efforts and analyses for this project was submitted to the BLM (Pastor et al. 2012). The objectives were accomplished by first conducting the file searches at the various state and federal agencies through which the project passes, and second, by conducting an intensive pedestrian inventory of the proposed pipeline ROW, and its associated temporary use access roads and TUAs. With the exception of a few of the proposed access roads that were previously inventoried in 1998 during the MAPCO Pipeline, the entire project was inspected during the Class III inventory. Recommendations regarding the significance of the cultural resources located during the project are made using the criteria for determining eligibility for nomination for inclusion on the NRHP. The historic preservation laws mandating this cultural resource study specifically identify eligibility to the National Register of Historic Places as the key factor in determining preservation needs. The criteria for assessing site significance, as published in the U. S. Government Code of Federal Regulations (36 CFR 60) reads as follows: The quality of significance in American history, architecture, archeology, engineering, and culture is present in districts, sites, buildings, structures, and objects that possess integrity of location, design, setting, materials, and workmanship, feeling, and association and 18 (a) that are associated with events that have made a significant contribution to the broad patterns of our history; or (b) that are associated with the lives of persons significant in out past; or (c) that embody the distinctive characteristics of a type, period, or method of construction, or that represent the work of a master, or that possess high artistic values, or that represent a significant and distinguishable entity whose components may lack individual distinction; or (d) that have yielded, or may be likely to yield, information important in prehistory or history. Identification and evaluation of cultural resources in the project area permits formulation of management recommendations. Management options for sites eligible for inclusion on the NRHP may include site avoidance or archaeological data recovery. Although an isolated find or feature may be determined to be eligible, they are typically considered to be insignificant and do not meet the requirements for inclusion on the NRHP and are not recommended for further treatment. FIELD AND LAB METHODS The Class III archaeological inventory was conducted by WAS along the entire pipeline route. The archaeological field methods employed during the field inventory were designed to efficiently locate all visible cultural resources within the project area and to collect the types of data required to assess site significant. Prior to the initiation of the survey, the pipeline corridor as divided into segments that extended between exiting roads providing access into the pipeline corridor, or other easy to identify landmarks. Within Colorado, the length of the segments varied up to 3 miles in length and reflected both the difficulty of the terrain and the distance that the crew might inventory in a day. Maps showing the location of previously documented cultural sites and the associated site records where compiled for each segment. Field notes were taken recording the location of both previously documented and newly recorded cultural resources, as well as notes on the local environment. Isolated artifacts were documented during the course of the pedestrian survey, with U.T.M. points saved as way points on a hand held GPS and GIS shape files recorded on a handheld Trimble. Locational information for both the previously documented sites and newly recorded sites were saved, with the crews returning later to fully document the site. After completion of the pedestrian survey, a visual analysis was conducted along the proposed pipeline ROW, with the analysis conducted at all NRHP eligible sites located within the nearby vicinity of the project area. The visual analysis was conducted primarily along eligible linear properties located within the project area, including contributing segments of the Uintah and D & RG Railroads, historic towns, ranches, roads, and other historic properties determined to be significant. Prehistoric sites that visual analysis was conducted at significant or potentially significant traditional cultural properties including prehistoric rock art sites and rock shelters. Pipeline construction will take place within a 100 ft wide zone, divided into a 75 ft wide working area and a 25 ft wide spoil pile area. Standard WAS methodology was used to conduct the inventory. A 200 ft wide (61 meters) ROW was inventoried along the proposed pipeline in northwestern Colorado. The ROW consisted of 150 ft (46 meters) inventoried on the working side of the centerline, and 50 ft (15 meters) inventoried on the non -working side. This insured the inventory of the actual construction zone, with a buffer on either side of the construction zone. 19 In addition to the pipeline ROW, 26 TUAs and 16 temporary use access roads were inventoried in northwestern Colorado. The TUAs varied widely in their size and dimensions, depending on the specific requirements of the individual TUA. Although nearly all of the proposed TUAs are located partially within the pipeline ROW, portions of all but four TUAs extended outside of the pipeline ROW and required additional inventory to provide the required 50 ft (15 meter) wide buffer zone. The shape files for each of the TUAs was downloaded into the hand held Trimble and used to located the boundaries of the TUAs. All of the 16 proposed temporary access roads extend partially outside of the 200 ft wide pipeline ROW. A 100 ft wide ROW was inventoried along the portions of the 16 new access roads located outside of the pipeline ROW, 50 ft (15 meters) to either side of the proposed access road. Survey crews consisted of two to five archaeologists walking parallel transects across the project area, spaced at 10 to 15 meter intervals. The archaeologists inspected the ground surface and erosional features within the project area for artifacts and cultural features. Where present, subsurface deposition exposed in stream cut banks, road cuts, pipeline disturbances, animal burrows, or animal trails were examined. Ant hills were examined for the presence of micro-artifacts including pressure flakes or small beads. Bedrock exposures were also closely examined for prehistoric rock art, historic inscriptions, rock shelters, and burials. Sites were defined as the locus of previous (50 year age minimum) human activity at which the preponderance of evidence suggests either one-time diagnostically interpretable use or repeated use over time, or multiple classes of activities. An isolate as defined by the BLM refers to one or more culturally modified object(s) not found in the context of a site. Locations of artifacts greater than 50 years in age, but not meeting the criteria for site definition, were recorded as isolated finds. Previously recorded sites believed to be within, or in close proximity to the project area were searched for, and information about them updated on the Colorado Cultural Resource Survey (CCRS) Forms if they were found to be within the survey area, with updated site sketches, inventories, and/or feature descriptions completed. Previously recorded information about the site was compared to the site's current condition and the site significance re-evaluated. In several instances, previously recorded sites could not be relocated and may have been destroyed by previous pipeline construction or other local developments or had been misplotted. Updates to the CCRS Forms were also completed for sites located outside of the survey area on which visual analysis was conducted. However, since these sites lie outside the survey corridor, site sketches and artifact inventories were not completed. When an artifact or cultural feature was encountered, the field crews intensively inspected the surrounding area to determine whether a site or an isolated find was represented. Newly recorded sites and isolated finds were assigned temporary field numbers, which included the WAS project number with a sequential site or isolate number. Efforts were made to determine the actual site boundaries, even if they extended some distance beyond the project centerline. WAS site field forms containing all of the pertinent information were completed in the field. At all of the site locations, a field sketch map was produced showing the site attributes, including tools, features, and structures, in relation to the proposed project and existing disturbance areas. A permanent site datum consisting of a 3/4" white PVC tube with a metal/foil tag marked with the temporary site number was placed at all of the new sites. Attempts were made to relocate the datums at previously recorded sites. If the datum could be relocated, a new datum was placed on the site. If the site size permitted, the datums were placed outside of the construction zone. A metal/foil tag marked with the temporary site number was affixed to the datum. UTM points recorded for the site datums and/or the center point of the isolated artifacts. GIS shape files were created showing the boundaries of the sites and 20 isolated artifacts. Site overview photographs were taken to aid in relocating the site, with photographs taken of all features and tools. Attempts were made to located (or relocate on previously documented sites) all surface features and formal tools. Non-diagnostic artifacts were analyzed and photographed in the field and were not collected. Diagnostic artifacts, such as ceramics and complete projectile points were collected. An inventory of all of the lithic debris found on the sites was recorded, including the quantity, stage of reduction, material type, and evidence of utilization. As per the BLM stipulations, site evaluations were limited primarily to surface observations and the use ofpin flag probes to determine soil depth where eolian deposits were present. Evaluative testing was conducted at one site (5ME423), where three 1 x 1 meter test units were excavated to recover a surface feature and to assess soil deposition. The testing was conducted in consultation with Aline LaForge of the Colorado BLM, Grand Junction Field Office. All fill from the test units were screen with 1/4" wire mesh screen. Two gallons of fill were collected from the site, with one gallon submitted for radiocarbon dating and the second gallon subjected to flotation analysis. The laboratory phase consisted of preparing site and isolate forms. Some of both the previously recorded and newly documented historic sites, including the homesteads, irrigation ditches, and historic inscriptions, required additional historical information to be gathered to put them in their proper context. Research was conducted online using the GLO records available on the BLM web site, the U.S. Census data, and water appropriations records from the Colorado Water Conservation Board and Colorado Division of Water Resources. Satellite photos from Google Earth were utilized to help in tracking down the locations of historic linear properties. RESULTS A total of 23 previously recorded sites and 9 newly recorded sites was recorded in Garfield County as a result of this project (Table 3). SUMMARY AND RECOMMENDATIONS The National Historic Preservation Act of 1966 (NHPA) directs that federal agencies protect cultural resources that possess significant values. Significance is a quality of cultural resource properties that qualifies them for inclusion in the NRHP. The statements of significance included in this report are field assessments that support management recommendations to the State Historic Preservation Officer (SHPO). The final determination of site significance is made by the controlling agency in consultation with the SHPO. The Code of Federal Regulations was used as a guide for site evaluations. Titles 36 CFR 50, 36 CFR 800, and 36 CFR 64 are concerned with the concepts of significance and (possible) historic value of cultural resources. Titles 36 CFR 65 and 36 CFR 66 provide standards for the conduct of significant and scientific data recovery activities. Finally, Title 36 CFR 60.6 establishes the measure of significance that is critical to the determination of a site's NRHP eligibility, which is used to assess a site's research potential: The quality of significance in American history, architecture, archaeology, and culture is present in districts, sites, buildings, structures, and objects of State and local importance that possess integrity of location, design, setting, materials, workmanship, feeling, and association, and a) that are associated with events that 21 have made a significant contribution to the broad patterns of history; or b) that are associated with the lives of persons significant in our past; or c) that embody the distinctive characteristics of a type, period, or method of construction, or that represent the work of a master, or that possess high artistic values, or that represent a significant and distinguishable entity whose components may lack individual distinction; or d) that have yielded, or may be likely to yield, information important in the prehistory or history. The eligibility determination and consultation process is guided by Section 106 of the NHPA (36 CFR 60, 63, and 800). Final determinations of National Register eligibility and effect are made by the controlling agencies in consultation with the State Historic Preservation Officer. The files search and intensive inventory indicated 33 cultural resources occur within the project area. A determination of "no adverse effect" for the project is recommended pursuant to Section 106 of the National Historic Preservation Act (36 CFR 800), however, final determinations of National Register eligibility and effect are made by the controlling agencies in consultation with the State Historic Preservation Officer. Although no significant portions of any prehistoric sites will be impacted by construction of the pipeline, a blading monitor and OTI are recommended for the entire pipeline due to the number of known sites along the pipeline route and in the general vicinity. In addition to the pipeline -wide blading monitor and OTI, several site-specific mitigation measures are recommended (see Table 3). Numerous historic sites were found during the project and a pattern of expansion in the region during the early nineteenth century was noted. Although the Colorado History: A Context for Historical Archaeology (Church et al.2007) Provides an excellent synthesis of the general themes in the project area, not all specific areas and historical occurrences are presented. A sub -regional Historic Context is recommended as part of mitigation for effects of the WEP II pipeline. REFERENCES CITED Athearn, Frederic J. 1982 An Isolated Empire: A History ofNorthwestern Colorado. Colorado Bureau of Land Management, Cultural Resources Series No. 2, 3' edition. Babcock, Thomas F., and James V. Sciscenti 1981 Archaeological Monitor of the MAPCO Rocky Mountain Liquid Hydrocarbons Pipeline: Bureau of Land Management, Craig District, Colorado. 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Wandsnider, LuAnn 1997 The Roasted and the Boiled. In Journal of Anthropological Archaeology 16:1-48. Article No. AA970303. Willey, Gordon R., and Jeremy A. Sabloff 1980 A History of American Archaeology. Second Edition. H. Freeman and Company, San Francisco. 33 Woodward -Clyde Consultants 1980a Cultural Resource Inventory, MAPCO 's Rocky Mountain Liquid Hydrocarbons Pipeline, Southwestern Colorado. Woodward -Clyde Consultants, San Francisco. Submitted to the Office of Archaeology and Historic Preservation, Denver. 1980b Cultural Resource Inventory, MAPCO 's Rocky Mountain Liquid Hydrocarbons Pipeline, Northwestern Colorado. Woodward -Clyde Consultants, San Francisco. Submitted to the Office of Archaeology and Historic Preservation, Denver. 1980c Cultural Resource Inventory, MAPCO 's Rocky Mountain Liquid Hydrocarbons Pipeline, Utah. Woodward -Clyde Consultants, San Francisco. Submitted to the Office of Archaeology and Historic Preservation, Denver. 1983 Final Report, Cultural Resource Management Program, MAPCO 's Rocky Mountain Liquid Hydrocarbons Pipeline, Southwestern Colorado. Woodward -Clyde Consultants, San Francisco. Submitted to the Office of Archaeology and Historic Preservation, Denver. 34 FOR OFFICIAL USE ONLY: DISCLOSURE OF SITE LOCATION PROHIBITED (43CFR7.18) Western Archaeological - Services e = PROPOSED PIPELINE ■ = COMPRESSOR STATIONS Q = TOWNS = INTERSTATE 70 DRAGON STATION 1 — LOCAL HIGHWAY MACON = COUNTY LINES — COLORADO RIVER UINTA COUNTY THOMPSON CRESEN1. SPRINGS IIINCmSN GRAND COUNTY RIO BLANCO COUNTY ATS GARFIELD COUNTY MACK TH6MPSdN STATION MOAN rn LAMA FRII[TA GBANID JUNCTION MESA, COUNTY A/Enterpflse WEP II Plpellne 29e 200 MOS Figure 1. Map of the general project area. 36 Figure 2. Map of Enterprise WEP 11 project in Garfield County 0 Milepost Centerline Access Road Survey Boundary Entereprise WEP II Pipeline TUA Ownership BLM PRIVATE STATE e4 . ;,East Evacuation `.Creek.(1664). - 500 0 500 Meters N A 0.5 0 0.5 Miles n!Thi..=MWAIMBIE i d o! • • . 11 NINIiIMEMIBB MS 1211911.111111 II MIWINEMIIM=MM intwimminzmuse r'iaCv -Y rI1 )CES• . Es ni+ua ' Nomisoen� nom mow: IIIMIIIIIMEM LIWIllirliaMiNEBBIlli -I OMB=! ..7L MEOW EMS= MIf,,;:/.m1111: Figure 3. Map of Enterprise WEP 11 project in Garfield County „ NB= =MEM= ENSIMM EllIMEMMIE =AM!MIM 1=11EN=IIMININ =5MEMEW.EI 111HIIRNEMMII NEMMEM IONENE=IIMMO Win= =MIME IMEMI •=i151= MNIMMIENIME IMIIIEMMENEM simmmm.• minum IMMIMIMICIEME NIMEMEM•wm . • ` : : , • ..•?( _..--,. • • ' • • • `• • '• ? fr7 ';•;•.;. • e - 1 1 7, 0.5 - 5 ) • • ,: • ••• • ••••• ••• „ • . • • • • •_-.7 • . • • •• „ ,-• , • ••• . • 1 • I ...I • ••-‘. • '- • ••••• I ' ; • . • , . , ; • 7, : „ „ • rds. 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I L' • T. .r.-,. .....--, , i .4, i ' dr d. ...., . __..'' • 15‘......;V: ir---......., 7--.-"-d -- •• / J \ .d. , r. d•.. - Li ) - • rI? \ ( . -- ..;"-• / d '':i V \/--'' 1:- [-- I .',” :1-0.\ r ---t ....,,,' ---,' ..,-P - ''--,-- '-,,) I 1 ''',, .• A, • •.. - 4? T1 ,,,,, ''-.1— -, ..7.-Y • I ...---, .: - • •- -- ,_ -...-:. r... ............ ,.../ 1 ,.. _ cb07 (198ip..:,..c9.73),,.:.'-:,,;-/!y7r ..2.,../frLT, — 77 • ' ' • 968) /I- _ ..., . c....... 2 • •• ••• .• /1 - -• •-•-••-•-• ••‘Th , ...,.. -..,.._ :E, likIli ....Af ° i .. . ._ , .,, -,- ...,.:- •._/ ••;,. 1. '' ' .i" • . •‘:•• .(.. - , • , ( 0 0 \ R1 aim._ Table 1. Previous cultural resource inventories in Garfield County. PROJECT AUTHOR YEAR CONTRACTOR Northwest Pipeline Corporation: System Expansion Project, CRI Unspecified Unspecified Unlisted Archaeological Survey of the Western Slope Company's Baxter Compressor Station Loop Line, Garfield County, Colorado Jennings, C. H. 1976 Colorado State University Laboratory of Public Archaeology Archaeological Reconnaissance of 13 Well Sites in the Book Cliffs Area, Garfield County, Colorado and Grand County, Utah dickens, P. R. 1977 University of Colorado Natural Gas Well Sites Nickens, P. R. 1977 University of Colorado Archaeological Reconnaissance of Three Gas Well Sites, Southwestern Garfield County, Colorado Nickens, P. R. 1977 University of Colorado Field Checks for Well Sites and Access Road, Garfield County, Colorado (Fed wells 12-16 & 21-16 Palmer Oil and Gas Co) Breternitz, D. A. 1977 University of Colorado Palmer Gas and Oil Co: Archaeological Reconnaissance of Thirteen Proposed Well Sites in the Book Cliffs Area, Garfield County and Grand CountyNickens, P. R. 1977 University of Colorado Archaeological Clearance Report for 18 Well Sites and Adjoining ROWs, Rio Blanco and Garfield Counties, Colorado Ryan, R. P. 1978 Centuries Research Veco Drilling: Drilling Rig Stack Location Unspecified 1979 BLM ROW of Lateral A-14 with USA 1-13 Well Kranzush, K. 1979 BLM 'rovident Government 2-33-5-102, Archaeological Survey of Well Pad and Proposed Access; CRI for Proposed Government 16-34-5-102 Well Pad, 3uffer Area and Access; and Survey for Government 2-20-5-102 Well Pad, Buffer Area and Access, Garfield County, Colorado Metcalf, M.. 1979 Powers Elevation Company Tenneco Oil Company 28-10 & 28-2 Federal, Archaeological Survey of Well Pad and Access, Garfield County, Colorado Metcalf, M. 1979 Powers Elevation Company Archaeological Clearance Survey of Seven Well Sites for Powers Elevation Company, Inc., In Garfield and Mesa Counties, Colorado Kvamme, K. L. 1979 Centuries Research Gas Pipeline in Northwest Colorado and East Central Utah Powers, M.A., and C. M. Haecker 1979 San Juan County Archaeological Research Center An Archaeological Survey of Gas Pipelines in Northwest Colorado and East Central Utah for Northwest Pipeline Corporation Powers, M.A., and C. M. Haecker 1979 San Juan County Archaeological Research Center An Intensive Inventory of Two Proposed Drill Holes in the Baxter Pass, Colorado Locality Smith, T. M. 1979 Archaeological Environment Research Corp West Central Colorado Coal Leases Final Report 1-1 ibbets, B. N. 1979 Archaeological Associates West Central Colorado Coal Leases, Garfield , Mesa, Gunnison, and Delta Counties, Colorado (Volumes 1-3) 1-iibbets, B. N., J. Grady, J. A. Halasi, H. Huse, and F. W. Eddy 1979 Archaeological Associates Texas Gas Exploration Corp: CRI of Five Proposed Well Sites/Access Roads (Fed # 14-2, 12-3, 21-4, 23-4, 31-16) Conner, C. E. 1979 Grand River Institute Three Proposed Gas Wells/Access Roads and a Pipeline (Govt #'s 34-2, 1-19-83, & 1-14-84) Euchner, J. 1980 BLM Lost Safari Reservoir Maintenance, Dam Maintenance, and Proposed Baxter Pass Catchment Apryll, K. 1980 BLM Mitchell Energy: Federal #2-34-7-104 Well Pad and Access Road Reed, A. D. 1980 BLM Determination of Eligibility: The Uintah Railway Mesa, Garfield, Rio Blanco Counties, Colorado Athearn, F. J., and S.F. Mehls 1980 BLM, State Office MAPCO Pipeline Right -of -Way Gazunis Schwennesen, K. 1980 BLM, Craig District Cultural Resources Survey of a Portion of Western Slope Gas Co. Fuelco B12, D12, P-29 Well Laterals, Tenneco 4" Gathering Line - 1980, and Tenneco 10-12 4" Well Lateral, Garfield County, Colorado Biggs, R. W. 1980 BLM, GJRA Management Appendices Grand Junction District Class I History Mehls, S. F. 1980 BLM, GJRA MAPCO's Rocky Mountain Liquid Hydrocarbons Pipeline Collins, S., and C. H. Jennings 1980 Woodward -Clyde Consultants A CRI MAPCO Hydrocarbons Pipeline- Northwestern Colorado Preliminary Report -Revised Collins, S., and C. H. Jennings 1980 Colorado State University Laboratory of Public Archaeology and Woodward -Clyde Consultants CRI MAPCO's Rocky Mountain Liquid Hydrocarbons Pipeline, NW CO Unspecified 1980 Woodward -Clyde Consultants CRI MAPCO's Rocky Mountain Liquid Hydrocarbons Pipeline, Southwestern, Colorado (Volume 1, Addendum I, II, and III) Fetterman, J. et al. 1980 Woodward -Clyde Consultants A Cultural Resource Inspection of Mitchell NRG Corporation's Proposed Fed 2-34-7-104, Located in Garfield County, Colorado Reed, A. D. 1980 dickens & Associates Woodward -Clyde Consultants: Archaeological Monitoring of the MAPCO Pipeline Construction between Carbonera and Baxter Pass Conner, C. E. 1980 Grand River Institute Archaeological Survey of Provident Resources Incorporated's Three Well Sites and Related Access Roads, Garfield County, Colorado Alexander, R. K. 1980 Grand River Consultants CRI of Two Northwest Pipeline Corporation Well Ties in the Rocky Mountain- South Canyon Gathering System, Garfield County, Colorado Alexander, R. K. 1980 Grand River Consultants CRI of Northwest Pipeline Corporations Well Tie with Texas Gas Explorations Federal 12-3 Garfield County, Colorado Alexander, R. K. 1980 Grand River Consultants Archaeological Survey of Devon Corporation's Fed 129 Road Realignments, Garfield County, Colorado Alexander, R. K. 1980 Grand River Consultants CRI of Northwest Pipeline Corporation, Lateral A-35 Pipeline and Well Tie 3-34-5-102, Foundation Creek Gathering System in Garfield County Alexander, R. K 1980 Grand River Consultants CRS for CIG Exploration , Inc. Proposed CIG 2-15-8-104 Well Pad and Access Road, Garfield County, Colorado Waitkus, B, R. 1980 Powers Elevation Company Cultural Resource Survey for Mitchell NRG Corporation Proposed Fed 3-11-8-104 Well Pad, Buffer Area, and Access, Garfield County, Colorado Watikus, B. R. 1980 Powers Elevation Archaeological Survey for CIG Exploration Proposed 2-17-8-104 Well Pad Location and Access, Garfield County, Colorado Waitkus, B. R. 1980 Powers Elevation 3elco Petroleum: Three Proposed Well Locations in Buttermilk Canyon (3-3, 8-3, and 9-10) Euchner, J. 1981 BLM ?owerline ROW for Moon Lake Electric for Horizons Communication Relay Station Garfield County, Colorado and Archaeological Survey of 250 T eet for the Proposed Extension of A Powerline for Mack Communications and Moon Lake Electric, Garfield County, Colorado Layhe, R. 1981 BLM, Craig District Coseka Reroute Access for 12-32-4-103 Well Knox, D. J. 1981 BLM, WRFO Survey of Proposed Coseka 12-32-4-103 Access Reroute Knox, D. J. 1981 BLM, WRFO Coseka Retoute Access for 12-32-4-103 Knox, D. J. 1981 BLM, WRFO ,uel Resources Development Company: Four Proposed Well Pads/Access Roads (F-1-6-104-S, F-33-6-103-S, L-23-6-104-S, M-20-6-103-S) in the 3axter Pass Area, Garfield County Conner, C. E. 1981 Grand River Institute UELCO/Beartooth Oil and Gas: CRI on a Proposed Access Road Realignment to Two Gas Wells in Garfield County Conner, C. E. 1981 Grand River Institute CRI Report on Proposed Well Location Buttermilk Canyon Unit No, 12-7 Federal, Garfield County for Belco Petroleum Corporation Conner, C. E. 1981 Grand River Institute Archaeological Monitor of the MAPCO Rocky Mountain Liquid Hydrocarbons Pipeline: BLM CD, Colorado (From Baxter Pass North to the Utah State Line) Babcock, T. F. and J. V. Sciscenti 1981 Grand River Consultants for Woodward- Clyde Consultants Monitoring Report - Spread 4: MAPCO Rocky Mountain Liquid Hydrocarbons Pipeline McEnany T. 1981 Woodward-Clyde Consultants Archaeological Survey of Northwest Pipeline Corporation's Reroute of Mitchell NRG's Fed 3-11 Well, Garfield County, Colorado Babcock, T. F. 1981 Grand River Consultants Archaeological Survey of Northwest Pipeline Corporation's Well Tie to Mitchell Federal 2-34-7-104, Garfield County, Colorado Babcock, T. F. 1981 Grand River Consultants Cultural Management Report, Federal 1-8 Well Pad and Access for Bearthooth Oil and Gas, Garfield County, Colorado O'Neil, B. 1981 Powers Elevation Company 3eartooth Oil and Gas: CRI of Federal 1-8 O'Neil, B. 1981 Powers Elevation Company 3eartooth Oil and Gas: CRI of Federal 13-3 Tate, M. 1981 Powers Elevation Company Cultural Resource Survey for the Beartooth Oil and Gas Fed 1-1 Well Pad and Access and Well Pad Fed 24-3, Garfield County, Colorado Oneil, B. 1981 Powers Elevation Company A Cultural Resource Survey for Beartooth Oil and Gas Company Fed 13-3, Fed 36-10, and Fed 29-13 Well Pads and Existing Access Requiring Upgrading and Improvement, Garfield County, Colorado Williams, G. E. 1981 Powers Elevation Company 3eartooth Oil and Gas: CRI of Federal 29-13 Williams, G. 1981 Powers Elevation Company 3eartooth Oil & Gas: CRI Report on Proposed Gas Well Federal #7-1 and Related Access Road in Garfield County Conner, C. E. 1982 Grand River Institute 3elco Development Corporation: Six Proposed Gas Wells (Atchee Unit Federal #'s 7-13, 9-5, 16-3, 8-21, 15-10, and Buttermilk Canyon Unit Federal 414-7) and Related Access Roads in Garfield County Wignall, C. M. 1982 Grand River Institute Archaeological Survey for Northwest Pipeline Corporations's Bar X South Canyon Second Exchange Point, Garfield County, Colorado Hartley, J. D. 1982 Grand River Consultants Archaeological Survey of Frontier Exploration, Seismic Shot Holes, Rat Hole Ridge, Garfield County, Colorado Sciscenti J. V., and D. M. Griffiths 1982 Grand River Consultants Northwest Pipeline Corporation, CRI of Texas Eastern Loop Pipeline Project (Appendix D,G,H, I, K) Unspecified 1983 Unlisted NW Pipeline Corp: CRI of the Texas Eastern Loop Pipeline Project (Appendix F) Unspecified 1983 Unlisted CRI of the Proposed Texas Eastern Pipeline Project, Western Co and Eastern Utah Fetterman, J. and L. Honeycutt 1983 Woods Canyon Archaeological Consultants The CRI of the Proposed Texas Eastern Pipeline Project, Western Colorado and Eastern Utah Fetterman, J.., and L. Honeycutt 1983 Woods Canyon Archaeological Consultants Texas East Pipeline Project West Colorado and East Utah Fetterman, J.., and L. Honeycutt 1983 Woods Canyon Archaeological Consultants CRMP: MAPCO's Rocky Mountain Liquid Hydrocarbons Pipeline Unspecified 1983 Woodward-Clyde Consultants Cultural Resource Survey for DYCO Mesagar: Federal #10-1 and 20-1 Garfield County abcock, T., and J. D. Hartley 1983 Grand River Consultants Archaeological Survey for Baxter Pass Road Reconstruction, Garfield County, Colorado for the Garfield County Road Department artley, J. D. 1983 Grand River Consultants Geophysical Service, Inc.: Archaeological Survey of Seismic Line 4493 T5S, R103W - Sections 25 and 36 Garfield County artley, J. D. 1983 Grand River Consultants Archaeological Survey of the Geophysical Svs Seismic Line 4493, Garfield and Rio Blanco Counties, Colorado abcock, T. F., and J. D. Hartley 1983 Grand River Consultants Garfield County Road Department: Archaeological Survey for Baxter Pass Road Reconstruction, Garfield County artley, J. D. 1983 Grand River Institute Archaeological Survey for Eight Seis Pros HeliPortable Lines in the Baxter Pass Area, Rio Blanco and Garfield Counties, Colorado ullivan, J. P. 1984 Grand River Consultants. CRI of 2.5 Acres for Road Relocation in Garfield County ight, B. 1985 BLM CRI for a Forestry/Wildlife Oak Cutting Project, Garfield County, Colorado igh, M. K. 1985 BLM, GJFO CRI Report on Approximately Four Miles of Proposed Pipeline and New Access in the Prarie/Buttermilk Canyons Area, Garfield County, Colorado :or D & G Roustabouts onner, C. E. 1985 Grand River Institute, Inc. CRI Proposed Pipeline Reroute Baxter Pass, Garfield County, Colorado Hammack L. C. 1985 Complete Archaeological Service Associates CRI Report on Proposed Fed Well Location 1 in Garfield County, Colorado Conner, C. E. 1987 Grand River Institute 7uelco: CRI on Proposed Federal Well Location I in Garfield County Conner, C. E. 1987 Grand River Institute CRI of The Proposed Fed 27-16 Well Location in Garfield County, Colorado for Lone Mountain Production Conner, C. E. 1989 Grand River Institute CRI of the New Frontier Seismic Line and Access Garfield County, Colorado and Uintah County, Utah Addendum Metcalf, M. 1989 Metcalf Archaeological Consultants. Northwest Pipeline Corporations Mainline Expansion Project: Class I Inventory Conducted for Eastern Utah and Western Colorado Unspecified 1990 Woods Canyon Archaeological Consultants Class I Northwest Pipeline Corporation's Mainline Expansion Project Eastern Utah and Western Colorado (SJ90100) Fetterman, J., S. Eininger and L. Honeycutt 1990 Woods Canyon Archaeological Consultants CRI Report on the Proposed Fed 23-6 & Fed 26-4 Well Locations in Garfield County, Colorado for Lone Mountain Production Conner, C. E. 1990 Grand River Institute -one Mountain Production: CRI on the Proposed Fed #23-6 and 26-4 Well Locations in Garfield County Conner, C. E. 1990 Grand River Institute CRI of Mitchell NRG Corporation's Proposed Well Pad, Bittercreek Unit 1-25-14-25 and Associated Access Roads in Uintah County, Utah and Garfield County, Colorado, Addendum Crum, S. 1990 Alpine Archaeological Consultants. Archaeological Monitoring of Northwest Pipeline Corporation's Evacuation Creek Underground Pipeline Montgomery, J. 1991 Abajo Archaeology Northwest Pipeline Corporation, System Expansion Project Class III CRI (2 Volumes) Honeycutt, L., and J. Fetterman 1991 Woods Canyon Archaeological Consultants CRI Report on the Proposed Pipeline to Fed 33-8 Well Location in Garfield County, Colorado for Lone Mountain Production Connner, C. E. 1991 Grand River Institute ?rairie Canyon Ponds 3 & 4, Garfield County, Colorado Deaver, D. 1992 BLM, GJFO CRI Report on the Proposed Dam and Drainage Project in Garfield County, Colorado for WestGas Hutchins, R. L. 1992 Grand River Institute The Archaeology of the Grand Junction Resource Area Crossroads to the Colorado Plateau and the Southern Rocky Mountains. A Class I Overview O'Neil, B. 1993 BLM, GJFO CRI Report on the Proposed Pipeline to the Fed #2-10-84 Well Location in Garfield County, Colorado for National Fuel Corporation Conner, C. E. 1993 Grand River Institute CRI Report on the Proposed Relocated Fed 34-26 Well Location and Related New Access in Garfield County, Colorado for National Fuel Corporation Conner, C. E. 1994 Grand River Institute CRI Report on the Proposed Fed 34-26 Well Location in Garfield County, Colorado for National Fuel Corp Conner, C. E. 1994 Grand River Institute CR Management Report GASCO Inc, Farney Fed 3-1 Well Location and Access Road, Garfield County, Colorado Tucker, G. C., . 1994 Powers Elevation Company CN Production Company: CRI for five Proposed Well Locations in the West Salt Creek and Prairie Canyon Areas of Garfield County Conner, C. E. 1995 Grand River Institute CRI Report for Five Proposed Well Locations in the West Salt Creek & Prarie Canyon Areas of Garfield County, Colorado For KN Production Company (S#9575) Conner, C. E. 1995 Grand River Institute �I Report for the Proposed Baxter Pass Fed 11-7 Well Location and Related Access in Garfield County, Colorado for KN Production Company Original and Addendum) Conner, C. E. 1995 Grand River Institute CRI Report on the Proposed Trail Canyon 31-7+5-103 Well Location and Access in Garfield County, Colorado for Amoco Production Co Conner, C. E. 1995 Grand River Institute CRI of Proposed Repeater Site for Northwest Pipeline Corporation, Garfield County, Colorado Fetterman, J. 1996 Woods Canyon Archaeological Consultants. CRI of Proposed Gas Pipelines in East Branch of the West Salt Creek, Garfield County, Colorado Montgomery, K. R. 1997 Montgomery Archaeological Consultants Class III CRI for the Proposed South Canyon Fed 10-11 Well Location on Federal Lands in Garfield County, Colorado for Tom Brown Inc. Conner, C. E. 1997 Grand River Institute Class III CRI Report on the Proposed South Canyon Federal 7-13 Well in Garfield County, Colorado (9712) Conner, C. E., and B. J. Davenport 1997 Grand River Institute Class III CRI for the Proposed 2.7 Mile Long 4' Pipeline to the Existing Atchee 15-10 Federal Well Location in Garfield County, Colorado Conner, C. E. 1997 Grand River Institute Class III CRI for the Proposed South Canyon Fed 10-11 Well Location and Access on Federal Lands in Garfield County, Colorado for Tom Brown nc. Conner, C. E 1997 Grand River Institute CRI of Mid-America Pipeline Company's Proposed Rock Mountain Expansion Project- Colorado Part 1 of 2: Mesa, Garfield & Rio Blanco Counties, Northwestern Colorado Horn, J. C„ S.M. Chandler, K. Redman, D. Langdon, D. Perry, and A. D Reed 1998 Alpine Archaeological Consultants Mid-America Pipeline Co: CRI of Access Roads, Reroutes, and TUA Associated with the Construction of the Rocky Mountain Expansion Loop PPL Unspecified 1998 Alpine Archaeological Consultants lithnographic Survey of the Proposed Mid-America Pipeline Company's Rocky Mountain Expansion Project Northwestern New Mexico, Western Colorado and Eastern Utah, Addendum: Second Hopi Letter Report Perlman, S. E. 1998 SWCA for Alpine Archaeological Consultants Class III CRI Report for the Proposed Fed 27-12 Well Location in Garfield County, Colorado for Hallwood Petroleum, Inc. Conner, C. E 1998 Grand River Institute CRI of Access Roads, Reroutes, and TUAs Associated with the Construction of the Mid-America Pipeline Company's Rocky Mountain Expansion i,00p Pipeline, Garfield, La Plata, Montezuma and Rio Blanco Counties, Colorado Davis, J. 1999 Alpine Archaeological Consultants Colorado Prehistory: A Context for the Northern Colorado River Basin, Multiple Counties (SHF 1997-P1-015) Reed, A. D., and M. Metcalf 1999 Alpine Archaeological Consultants and Metcalf Archaeological Consultants Extensive Data Recovery Plan for Mid-America Pipeline Company's Proposed Rocky Mountain Expansion Project, Western Colorado, Eastern Utah & Northwestern New Mexico Horn, J. C.,, A. D. Reed, J. Fetterman and L. Honeycutt 1999 Alpine Archaeological Consultants and Woodward -Clyde Consultants Migrations in the North: Hopi Reconnaissance for the Rocky Mountain Expansion Loop Pipeline Anyon, R. 1999 Heritage Resources Management Consultants, LLC w/ Hopi Cultural Preservation Office for SWCA CRI of Hallwood Petroleum's Seven Well Locations in the Prairie Canyon Area, Garfield County, Colorado Montgomery, K. R., and S. Kinear-Ferris 2000 Montgomery Archaeological Consultants CRI Report Range Permit Renewal for the Year 2000: Evaluation of Grazing Impacts in Mesa and Garfield Counties, Colorado for the BLM GJFO Conner, C. E., and B. J. Davenport 2000 Grand River Institute ^.,evel II Documentation of Fourteen Segments fo the Uintah Railroad Grade (5ME767/5GF642/5RB823) Mesa, Garfield, and Rio Blanco Counties, Colorado Horn, J C. 2001 Alpine Archaeological Consultants The Mid-America Pipeline Company/Williams Rocky Mountain Expansion Loop Pipeline Archaeological Data Recovery Project Northwestern New Mexico, Western Colorado, and Eastern Utah Chapters 5, 19-22 (Limited Data Recovery/Monitoring, 5GF620, 5LP2345, 5ME422, Horn, J. C., J. Fetterman, and L. Honeycutt 2002 Alpine Archaeological Consultants and Woods Canyon Archaeological Consultants The Mid-America Pipeline Company/Williams Rocky Mountain Expansion Loop Pipeline Archaeological Data Recovery Project Northwestern New Mexico, Western Colorado and Eastern Utah Volumes 1-7 (Draft) Horn, J. C., J. Fetterman, and L. Honeycutt 2002 Alpine Archaeological Consultants and Woods Canyon Archaeological Consultants The Mid-America Pipeline Company/Williams Rock Mountain Expansion Loop Pipeline Archaeological Data Recovery Project Northwestern New Mexico, Western Colorado and Eastern Utah Chapters 25, 26 (5DL318, 5GF1561) Horn, J. C., J. Fetterman, and L. Honeycutt 2002 Alpine Archaeological Consultants and Woods Canyon Archaeological Consultants The Mid-America Pipeline Company Proposed Rocky Mountain Expansion Loop Pipeline Archaeological Data Recovery Project Fetterman, J. and L. Honeycutt 2003 Alpine Archaeological Consultants Tracing the Past Archaeology Along the Rocky Mountain Expansion Loop Pipeline Cassells. E S. 2003 Alpine Archaeological Consultants The Mid-America Pipeline Company/Williams Rocky Mountain Expansion Loop Pipeline Archaeological Data Recovery Project Northwestern New Mexico, Western Colorado and Eastern Utah Chapter 27 (5GF1562) Horn, J. C., J. Fetterman, and L. Honeycutt 2003 Alpine Archaeological Consultants and Woods Canyon Archaeological Consultants _ Class III CRI of the Buniger and Spring Canyon Ponds Range Improvement Project in Garfield County, Colorado Darnell, N. M. 2004 BLM, GJFO Evergreen Resources Inc. Class III CRI of Two Columbine Springs Fed Well Pads, Access Roads and Pipelines in Garfield County, Colorado Metcalf, M. 2004 Metcalf Archaeological Consultants Class III CRI of Canyon Gas Resources San Arroyo to South Canyon Pipeline Garfield County and Grand County, Utah (MOAC No. 04-225): Addendum: CRI of the San Arroyo to South Canyon Rerouted Pipeline, Garfield County, Colorado Bond, M. C.., and J. A. Montgomery 2004 Montgomery Archaeological Consultants. Class III CRI for Proposed Gathering Pipelines to Fed Wells 1-34, 1-35, 2-34, & 12-3 for National Fuel Corporation in Garfield County, Colorado Conner, C. E. 2004 Grand River Institute ?aleo investigation of ROW for Canyon Gas Resources Pipeline near Baxter Pass Unspecified 2005 Robert Young Class III CRI of the Hazzard 6-1 Well Pad and Access Road, Rio Blanco and Garfield Counties, Colorado Baeh, S., H. Guy Hays, and M.Retter 2005 SWCA Class III CRI for the West Salt Vegetation Treatment Project in Garfield County, Colorado for the BLM GJFO Conner, C. E., and B. J. Davenport 2005 Grand River Institute Class III CRI for Two Proposed Pipeline Routes for CDX High Inert Project (Snow Grove Mesa 30-5-103 and CDX Govt Buttram #1) in Garfield County, Colorado Conner, C. E. 2005 Grand River Institute CRI of the East Tavaputs Plateau Aspen Rejuvenation Project, A Sample Inventory of 418 Acres Located in Garfield County, Colorado (06-81-01) Dussinger, M. 2006 BLM, VFO CRI of the Meeker Lateral Pipeline, Rio Blanco and Garfield Counties Greenberg, M., and C. Kester- Tallman 2006 Cultural Resource Analysts Final Report: Colorado Radiocarbon Database Project, Multiple Counties (SHF 2005-M2-003) Berry, C. F. 2006 Dominguez Archaeological Research Group. A CRI of the Uinta Broadcasting Tower Near Baxter Pass, Garfield County, Colorado Johnson, W. S. 2007 Sagebrush Archaeological Consultants A CRI of the Uinta Broadcasting Tower Line Near Baxter Pass, Garfield County, Colorado Weymouth, H. M. 2007 Sagebrush Archaeological Consultants Williams Northwest Pipeline Vernal District: CRI of Two Locations, Garfield County Smith, C.,, B. Hill, D. Byers 2008 ENTRIX, INC. A CRI of Retamco's Proposed Rathole Gathering Area Pipeline and Access Roads in Garfield County, Colorado Johnson, W. S. 2009 Sagebrush Archaeological Consultants A CRI for the Proposed Badger Wash 2-D Seismic Lines BW -2008-1 thru 5 and Seismic Line DC -2008-1 and Its Associated Access Roads, Mesa and Garfield Counties, Colorado (BLM NO. 5508-02) Pagano, S. C. 2009 Sagebrush Archaeological Consultants Class III CRI of 67 Anomaly and Recoat Locations, Rangely to Cisco, Williams Northwest PPL, Garfield and Mesa Counties, Colorado Hill, B. L., C. S. Smith and Z. 2010 Entrix, Inc. 1\Telson Table 2. Previously documented cultural resources in Garfield County. SITF CUT TIIRF TYPF FI.IGIRII.ITV FIELD OFFIUF T/R SF('TI4)\\ LAND OWNFR CONTRACTOR YF,AR BEARING DISTANCE Meters GARFIELD COUNTY 5GF139 Prehistoric isolated find Not Eligible (field) GJFO 8S/104W 10 BLM BLM 1979 IN (SE) 10 5GF140 Prehistoric isolated find Not Eligible (field) GJFO 8S/104W 10 BLM BLM 1979 E 75 5GF162 Prehistoric isolated find Not Eligible (field) GJFO 6S/104W 0 BLM AA 1978 W 265 5GF221 Historic trash dump Not Eligible (field) GJFO 7S/104W 10 BLM BLM 1977 SW 1640 5GF223 Historic camp Not Eligible (field) GJFO 7S/104W 15 BLM BAR 1977 W 1650 5GF271 Multi component sheltered lithic/trash dump Not Eligible (official) GJFO 6S/103W 35 BLM GRI 1995 IN (NW) 45 5GF332 Multi component rock art Not Eligible (field) GJFO 7S/104W 28 BLM BLM 1977 NW 735 5GF333 Prehistoric rock art Not Eligible (field) GJFO 7S/104W 27 BLM BLM 1977 NW 195 5GF341 Prehistoric sheltered camp Needs Data GJFO 7S/104W 27 BLM GRI 1977 NW 250 5GF342 Prehistoric rock art Needs Data GJFO 7S/104W 23 BLM GRI 1977 NW 100 5GF395 Historic foundation Not Eligible (official) GJFO 7S/104W 27 BLM GRI 1998 NW 285 5GF399 Historic camp Not Eligible (field) GJFO 7S/104W 27 BLM HMIWC 1977 NW 445 5GF466 Historic habitation Needs Data GJFO 5S/103W 6, 7 Private GRI 1995 W 115 5GF518 Prehistoric rock art Not Eligible (field) GJFO 7S/104W 23 BLM CAS 1979 NW 70 5GF605 Prehistoric isolated find Not Eligible (field) GJFO 5S/103W 8 Private LOPA 1980 IN (SW) 20 5GF619 Prehistoric rock art, open camp Eligible (official) GJFO 6S/103W 35 Private ALP 1998 NW 75 5GF620 Multi component open camp/trash Eligible (official) GJFO 6S/103W 7,12 Private CRA 2005 IN -- 5GF621 Historic trail/road Needs Data GJFO 5S/103W 27, 34, 35 Private SWCA 2006 IN -- 5GF621.1 Historic trail/road Needs Data GJFO 5S/103W 27, 34, 35 Private/BLM ALP 1998 IN -- 5GF622 Historic inscriptions Needs Data GJFO 5S/103W 34 Private/BLM SWCA 2006 NE 250 5GF623 Historical isolated find Not Eligible (field) GJFO 6S/103W Unsectioned BLM GRI 1980 E 75 5GF625 Prehistoric isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private GRI 1980 S 50 5GF626 Prehistoric isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private GRI 1980 SE 95 5GF627 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private GRI 1980 IN (NE) 25 5GF628 Prehistoric isolated find Not Eligible (field) GJFO 6S/1 -3W Unsectioned Private GRI 1980 SW 70 5GF629 Prehistoric isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private GRI 1980 SW 60 5GF630 Multi component isolated find Not Eligible (field) GJFO 5S/103W 35 Private GRI 1980 IN (SW) 10 5GF631 Historic isolated find Not Eligible (field) GJFO 5S/103W 35 Private GRI 1980 IN (SW) 10 5GF632 Prehistoric isolated find Not Eligible (field) GJFO 6S/104W Unsectioned BLM GRI 1980 NNW 40 5GF633 Prehistoric isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private GRI 1980 NW 120 5GF634 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned BLM GRI 1980 IN -- 5GF635 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned BLM GRI 1980 IN -- 5GF636 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned BLM GRI 1980 E 85 5GF637 Historic isolated find Not Eligible (field) GJFO 6S/104W Unsectioned Private GRI 1980 E 95 5GF638 Historic isolated find Not Eligible (field) GJFO 5S/103W 34 BLM GRI 1980 N 140 5GF639 Historic isolated find Not Eligible (field) GJFO 5S/103W 34 BLM GRI 1980 N 400 5GF640 Historic homestead Eligible (official) GJFO 7S/104W 2, 3 Private/BLM CRA 2006 IN -- 5GF641 Historic cairn Not Eligible (field) GJFO 5S/103W 34 BLM GRI 1980 S 115 5GF642 Historic railroad Eligible 1 GJFO 5S/103W multiple Private/BLM WCRM 1991 IN -- 5GF642.1 Historic railroad Eligible (non-contributing) GJFO 7S/104W 14 Private 1980 IN -- 5GF642.2 Historic town Eligible (contributing) GJFO 6S/103W multiple Private BLM 2011 E 80 5GF642.3 Historic railroad Eli ible (contributing) GJFO 8S/104W 15 BLM ALP 1998 E 270 5GF642.4 Historic railroad Eligible (contributing) GJFO 8S/104W 3, 10 Private/BLM ALP 1998 W 75 5GF642.5 Historic railroad Eligible (contributing) GJFO 6S/103W multiple Private/BLM ALP 1998 (IN) E 25 5GF642.6 Historic railroad Eligible (contributing) GJFO 6s/103w 35 Private/BLM ALP 1998 IN -- 5GF642.7 Historic railroad Eligible (non-contributing) GJFO 5S/103W 16, 21, 22, 27, 28, 33, 34 Private/BLM ALP 1998 IN -- 5GF642.8 Historic railroad Eligible (non-contributing) GJFO 5S/103W 21 Private ALP 1998 IN (E) 25 5GF642.9 Historic railroad Eligible (non-contributing) GJFO 5S/103W 6; 5, 8, 17, 20, 21 Private/BLM ALP 1998 IN -- 5GF642.10 Historic railroad Eligible (contributing) GJFO 6S/103W multiple Private ALP 1998 IN -- 5GF642.11 Historic railroad Eligible (contributing) GJFO 6S/103W 6S/104W multiple Private/BLM CRA 2006 IN -- 5GF642.12 Historic railroad Eligible (contributing) GJFO 8S/104W 3 Private/BLM MONT 2004 E 345 5GF642.13 Historic railroad Eligible (contributing) GJFO 6S/103W multiple Private/BLM CRA 2006 E 100 5GF740 Historic industrial Not Eligible (official) GJFO 5S/103W 21 Private/BLM WOOD 1980 E W 150 145 5GF744 Historic isolated find Not Eligible (field) GJFO 6S/104W 0 Private CRA 2005 (IN)W 25 5GF852 Prehistoric rock art Not Eligible (field) GJFO 5S/103W 5 Private GKAC 1981 E 250 5GF1110 Historic homestead Needs Data GJFO 6S/103W Unsectioned Private BLM 1982 W 85 5GF1125 Prehistoric isolated find Not Eligible (field) GJFO 6S/104W Unsectioned Unknown GRI 1980 W 2785 5GF1126 Prehistoric isolated find Not Eligible (field) GJFO 6S/104W Unsectioned Unknown GRI 1980 W 1425 5GF1127 Prehistoric open lithic Not Eligible (field) GJFO 8S/104W 10 Private WCAC 1982/1991 W 170 5GF1128 Prehistoric open architectural Eligible (field) GJFO 7S/104W 34 BLM WCAC 1982/1991 W 50 5GF1130 Historic farming/ranching Not Eligible (field) GJFO 6S/104W Unsectioned Private WCAC 1982 SW 2175 5GF1150 Prehistoric isolated find Not Eligible (field) GJFO 8S/104W 10 BLM WCAC 1982 NW 120 5GF1151 Historic isolated find Not Eligible (field) GJFO 7S/104W 34 BLM WCAC 1982 W 75 5GF1152 Historic isolated find Not Eligible (field) GJFO 7S/104W 27 BLM WCAC 1982 N 36 5GF1153 Prehistoric isolated find Not Eligible (field) GJFO 7S/104W 27 BLM WCAC 1982 N 90 5GF1154 Prehistoric isolated find Not Eligible (field) GJFO 7S/104W 11 Private NICK 1982 IN -- 5GF1155 Historic isolated find Not Eligible (field) GJFO 7S/104W 3 BLM WCAC 1982 SW 555 5GF1156 Historic isolated find Not Eligible (field) GJFO 6S/104W 12 Private WCAC 1982 NW 340 5GF1171 Prehistoric open camp Needs Data GJFO 7S/104W 34 BLM BLM 1983 W 180 5GF1436 Prehistoric rock art Not Eligible (field) GJFO 7S/104W 27 BLM BLM 1987 NW 145 5GF1459 Prehistoric open camp Unknown GJFO 7S/104W 27 BLM BLM 1988 SE 235 5GF1460 Prehistoric open architectural, ceremonial Eligible (official) GJFO 7S/104W 27 BLM BLM 1988/2000 SE 100 5GF1475 Historic camp Not Eligible (field) GJFO 8S/104W 10 BLM BLM 1980 E 1145 5GF1491 Prehistoric isolated find Not Eligible (field) GJFO 7S/104W 27 BLM GRI 1989 SE 555 5GF1561 Multi open lithic/homestead Eligible (official) GJFO 6S/104W 25 Private CRA 2005 W 25 component 5GF1562 Historic town Eligible (official) GJFO 6S/103W 11,14 Private CRA 2006 IN -- 5GF1563 Prehistoric isolated find Not Eligible (field) GJFO 6S/103W 7 BLM WCAC 1991 IN (E) 10 5GF1564 Historic isolated find Not Eligible (field) GJFO 6S/104W Unsectioned Private WCAC 1991 NW 110 5GF1577 Prehistoric open camp Needs Data GJFO 7S/104W 33 Private GRI 1991 W 590 5GF2121 Prehistoric rock art Eligible (official) GJFO 7S/104W 11 Private GRI 1994 NE 135 5GF2465 Prehistoric isolated find Not Eligible (field) GJFO 8S/104W 4 Private WCRM 1977 W 230 5GF2575.1 Historic trail/road Not Eligible (official) GFJO 5S/103W 21 Private/BLM WCRM 1979 IN (NE) 45 5GF2576 Historic isolated feature Not Eligible (field) GJFO 5S/103W 17 BLM ALP 1998 IN (W) 10 5GF2585 Historic isolated feature Not Eligible (field) GJFO 5S/103W 35 Private MAC 1998 IN (S) 45 5GF2700 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private ALP 1998 SE 50 5GF2701 Prehistoric open camp Eligible (field) GJFO 8S/104W 10 BLM ALP 1999 E 107 5GF2761 Prehistoric isolated find Not Eligible (field) GJFO 5S/103W 35 Private ALP 1999 S 90 5GF3823 Historic isolated find Not Eligible (field) GJFO 6S/104W 6 Private BLM 2005 -- -- 5GF3857 Historic trash dump Not Eligible (field) GJFO 7S/104W 14 Private CRA 2005 W 70 5GF3859 Historic trash dump Not Eligible (field) GJFO 6S/103W 6 Private CRA 2006 IN -- 5GF3861 Historic trash dump Not Eligible (field) GJFO 6S/103W 6 Private CRA 2006 IN -- 5GF3865 Prehistoric isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private/BLM CRA 2006 NE 110 5GF3867 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private CRA 2006 IN 45 5GF3868 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private CRA 2006 NE 90 5GF3869 Historic isolated find Not Eligible (field) GJFO 6S/103W Unsectioned Private CRA 2006 NE 55 5GF4027 Prehistoric isolated find Not Eligible (field) GJFO 7S/104W 10 Unknown UC 1977 5Ci-F40214 Prehistoric isolated find Not Fligihle (field) GTFO 7S/104W 10 RT.M ITC 1977 SW 1370 Table 3. Garfield County Sites in association with the WEP II pipeline project. Site No. Description NRNP Eligibility Land owner Impacts Recommendation Pipeline TUA Access 5GF271 Prehistoric rock shelter, Historic corral Not Eligible BLM No No po None 5GF620 Prehistoric open camp, Historic trash Eligible non contributing Private Yes No No Blading monitor and open trench inspection of pipeline 5GF621.1 Historic wagon road Eligible non contributing Private, BLM No No Yes None. Access road site on previously upgraded road, no upgrading is needed 5GF640 Historic ranch Eligible non contributing Private, BLM Yes Yes Yes Blading monitor and open trench inspection of pipeline. Barricade fence in area of Feature 4 5GF642.2 Historic Atchee townsite Eligible non contributing Private, BLM No Yes Yes TUA recommended dropped. Access to new TUA follows existing upgraded road through site, no upgrading is needed 5GF642.3 Uintah Railroad Eligible contributing Private, BLM No No No None 5GF642.4 Uintah Railroad Eligible non- contributing BLM Yes No No None. Previous construction destroyed 5GF642.5 Uintah Railroad Eligible contributing Private No No No None 5GF642.6 Uintah Railroad Eligible contributing Private No No No None 5GF642.7 Uintah Railroad Eligible non- contributing Private, BLM Yes No No None. The segment has been previously upgraded 5GF642.8 Uintah Railroad Eligible, non- contributing Private Yes No No None 5GF642.9 Uintah Railroad Eligible non- contributing Private, BLM Yes Yes Yes None. The grade has been previously upgraded 5GF642.10 Uintah Railroad Eligible contributing Private No No Yes None. An access road (AR57) follows a previously upgraded road across the segment. No upgrading is needed. 5GF642.11 Uintah Railroad Eligible contributing Private, BLM Yes No No Restrict construction to existing disturbance. Recontour and revegetate 5GF642.13 Uintah Railroad Eligible contributing BLM No No No None 5GF740 Historic water pipeline Eligible Private, BLM Yes No No Blading monitor and open trench inspection of pipeline. In consultation with Michael Selle of the BLM, White River Field Office, additional work was discussed to more precisely determine the exact location of the route. This would involve archival research at American Gilsonite (previous attempts to contact American Gilsonite were fruitless) to locate any available maps and use of a metal detector or line locator to attempt to located any remnants of the water line. Subsequent to the fieldwork, the landowner (Jon D. Hill) of the property in this area submitted a letter to Enterprise-MAPL denying any request to locate the water line on his land 5GF1561 Historic ranch Eligible Private, BLM No No No None 5GF1562 Historic Carbonera townsite Eligible Private Yes No No Restrict construction to existing disturbance. Recontour and revegetate 5GF2585 Historic telephone line Not Eligible Private, BLM Yes No No None 5GF2575.1 Historic wagon road Eligible Private No No No None 5GF2575.2 Historic wagon road Eligible non contributing Private Yes No No None 5GF3859 Historic trash scatter Not Eligible Private Yes No No None 5GF3861 Historic trash scatter Not Eligible Private No No No None 5GF4653 Historic irrigation ditch Eligible Private, BLM Yes No No Recontour/revegetate ditch 5GF4656 Prehistoric rock shelter Unevaluated BLM No No No None 5GF4660 Historic irrigation ditch Eligible BLM Yes No No Restrict construction to existing disturbance and fence ROW 5GF4664 Historic corral Not Eligible Private No No Yes None 5GF4667 Historic irrigation ditch Eligible Private Yes Yes Yes Recontour/revegetate ditch. Possible bore under ditch 5GF4668 Historic Windella water tower Eligible Private No Yes No Drop northwest corner of TUA 5GF4669 Historic homestead Prehistoric lithic scatter Eligible non contributing Private Yes No No Restrict construction to existing disturbance and fence ROW 5GF4671 Historic irrigation ditch Eligible Private, BLM Yes Yes No Recontour/revegetate ditch 5GF4685.1 Historic Mahaney's Ranch to Fruita Road Eligible non contributing Private, BLM Yes Yes Yes None. The site is an upgraded county road