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HomeMy WebLinkAboutApplication- PermitGARFIELD COUNTY BUILDING AND SANITATION DEPARTMENT 108 Eighth Street, Suite 201 Glenwood Springs, Coloradof 81601 Phone (970) 945-8212 INDIVIDUAL SEWAGE DISPOSAL PERMIT PROPERTY Owner's Name System Location Legal Description of Assessor's Parcel No SYSTEM DESIGN Permit 4012 Assessor's Parcel No. This does not constitute a building or use permit. resent Address&! 55te -k) Sb St QEhone31 9 389(c) 6, /- /ez 7/ OJO Lot IO tJa-Five. Sr fly atbct. Septic Tank Capacity (gallon) Other Percolation Rate (minutes/inch) Number of Bedrooms (or other) Required Absorption Area - See Attached Special Setback Requirements: Date Inspector FINAL SYSTEM INSPECTION AND APPROVAL (as installed) Call for Inspection (24 hours notice) Before Covering Installation System Installer Septic Tank Capacity Septic Tank Manufacturer or Trade Name Septic Tank Access within 8" of surface Absorption Area Absorption Area Type and/or Manufacturer or Trade Name Adequate compliance with County and State regulations/requirements Other Date 5/31 Inspector RETAIN WITH RECEIPT RECORDS AT CONSTRUCTION SITE CONDITIONS: 1. All installation must comply with all requirements of the Colorado State Board of Health Individual Sewage Disposal Systems Chapter 25, Article 10 C.R.S. 1973, Revised 1984. 2. This permit is valid only for connection to structures which have fully complied with County zoning and building requirements. Con- nection to or use with any dwelling or structures not approved by the Building and Zoning office shall automatically be a violation or a requirement of the permit and cause for both legal action and revocation of the permit. 3. Any person who constructs,alters, or installs an individual sewage disposal system in a manner which involves a knowing and material variation from the terms or specif ications contained in the application of permit commits a Class 1, Petty Offense ($500.00 fine — 6 months in jail or both). w6M ACCT I"ACm' v 0 no- n•rer.. I.... Me 0 y %prim _LS TS INDIVIDUAL SEWAGE DISPOSAL SYSTEM APPLICATION OWNER /CPC*. ADDRESS a� &.(11< )i i PHONE_ _ CONTRACTOR LLl 2' CMCO Qct c Q(_ ADDRESS ai5i 1?d a t 5 L4- PHONE R1Th'w) U call 319- 80/0 PERMIT REQUEST FOR NEW INSTALLATION ( ) ALTERATION ( ) REPAIR Attach separate sheets or report showing entire area with respect to surrounding areas, topography of area, habitable building, location of potable water wells, soil percolation test holes, soil profiles in test holes (See page 4). LOCATION OF PROPOSED FA(CILITY: Near what City of Town n Size ofLot 5. 17,Q hett Legal Description or Addres� itjcl� i tJP S prt Dr, , 1 t .Pcp , Co 206:17) WASTES TYPE: (tj/DWELLING ( ) COMMERCIAL OR INDUSTRIAL ( ) NON-DOMESTIC WASTES ( ) OTHER—DESCRIBE ( ) TRANSIENT USE BUILDING OR SERVICE TYPE: Si n � awJ\ u Number of Bedrooms 3 umber of Persons s _ ('4' Garbage Grinder (VcAutomatic Washer ( "Dishwasher SOURCE AND TYPE OF WATER SUPPLY: ( /WELL ( ) SPRING ( ) STREAM OR CREEK If supplied by Community Water, give name of supplier: DISTANCE TO NEAREST COMMUNITY SEWER SYSTEM: (L&oY) U ?FYI . Sprrp Was an effort made to connect to the Community System? Nj(n �3 rytki I A site plan is required to be submitted that indicates the following MINIMUM distances: Leach Field to Well: Septic Tank to Well: Leach Field to Irrigation Ditches, Stream or Water Course: Septic System (septic tank & disposal field) to Property Lines: 100 feet 50 feet 50 feet 10 feet YOUR INDIVIDUAL SEWAGE DISPOSAL SYSTEM PERMIT WILL NOT BE ISSUED WITHOUT A SITE PLAN. GROUND CONDITIONS: Depth to first Ground Water Table Percent Ground Slope • 7. r r TYPE OF INDIVIDUAL SEWAGE DISPOSAL SYSTEM PROPOSED: (t( SEPTIC TANK ( ) AERATION PLANT ( ) VAULT ( ) VAULT PRIVY ( ) COMPOSTING TOILET ( ) RECYCLING, POTABLE USE ( ) PIT PRIVY ( ) INCINERATION TOILET ( ) RECYCLING, OTHER USE ( ) CHEMICAL TOILET( ) OTHER -DESCRIBE FIN,L DISPOSAL BY: ( 16 ABSORPTION TRENCH, BED OR PIT ( ) EVAPOTRANSPIRATION ( ) UNDERGROUND DISPERSAL ( ) SAND FILTER ( ) ABOVE GROUND DISPERSAL ( ) WASTEWATER POND ( ) OTHER -DESCRIBE WILL EFFLUENT BE DISCHARGED DIRECTLY INTO WATERS OF THE STATE? PERCOLATION TEST RESULTS: (To be completed by Registered Professional Engineer, if the Engineer does the Percolation Test) Minutes per inch in hole No. 1 Minutes per inch in hole No. 3 Minutes per inch in hole No. 2 Minutes per inch in hole No. _ 4 ° Gwf e tk Name, address and tel one of RPE who made§941 absorption tests: 5bac� _P2154 G s Xi6or Name, address and telephone of RPE responsible for design of the system: (to -f e c`" 1 Applicant acknowledges that the completeness of the application is conditional upon such further mandatory and additional tests and reports as may be required by the local health department to be made and furnished by the applicant or by the local health department for purposed of the evaluation of the application; and the issuance of the permit is subject to such terms and conditions as deemed necessary to insure compliance with rules and regulations made, information and reports submitted herewith and required to be submitted by the applicant are or will be represented to be true and correct to the best of my knowledge and belief and are designed to be relied on by the local department of health in evaluating the same for purposes of issuing the permit applied for herein. I further understand that any falsification or misrepresentation may result in the denial of the application or revocation of any permit granted based upon said application and in legal action for perjury as provided by law. Signed CSCrt,l.A--nCii_./ Date g J I q C Li - PLEASE DRAW AN ACCURATE MAP TO YOUR PROPERTY!! 00'SLZ Co CO CO 91,92.00 N 235.00' , V- _ 235.00' .00 9z Z 1 3 « 61 92.00 S /V6i4 jr44Yartce s • I Gtech Aar kI' 10 Nal kit Sprior 'awe') 142402,01- No»Jo & Ouslopmeta Ccs•, CLc Hepworth-Pawlal: Geotechnical. Inc. 5020 Count.Road 154 Glenwood Springs, Colorado 81601 Phone: 970-945-7988 Pax: 970-945-8454 hpgeo@hpgeotech.com PRELIMINARY GEOTECHNICAL STUDY PROPOSED NATIVE SPRINGS SUBDIVISION COUNTY ROAD 221 GARFIELD COUNTY, COLORADO JOB NO. 100 460 JANUARY 16, 2001 PREPARED FOR: JIM AND PAUL LUGINBUHL P.O. BOX 950 BASALT, COLORADO 81621 TABLE OF CONTENTS PURPOSE AND SCOPE OF STUDY 1 PROPOSED DEVELOPMENT 1 SITE CONDITIONS GEOLOGIC SETTING FIELD EXPLORATION 3 S 11B SURFA CE CONDITIONS GEOLOGIC SITE ASSESSMENT 5 PRELIMINARY DESIGN RECOMMENDATIONS 6 FOUNDATIONS 6 FLOOR SLABS 7 UNDERDRAIN SYSTEM 7 SITE GRADING 7 SURFACE DRAINAGE 8 PERCOLATION TESTING 8 LIMITATIONS 8 REFERENCES 10 FIGURE 1 - GEOLOGY MAP AND BORING LOCATIONS FIGURES 2 & 3 - LOGS OF EXPLORATORY BORINGS FIGURE 4 - LEGEND AND NOTES FIGURES 5 & 6- SWELL -CONSOLIDATION TEST RESULTS TABLE I - SUMMARY OF LABORATORY TEST RESULTS TABLE II - PERCOLATION TEST RESULTS H -P GEOTECH PURPOSE SND SCOPE OF STUDY This report presents the results of a preliminary geotechnical study for the proposed Native Springs Subdivision, County Road 221, Garfield County, Colorado. The project site is shown on Fig. 1. The purpose of the study was to evaluate the geologic and subsurface conditions and their potential impacts on the project. The study was conducted in accordance with our proposal for geotechnical engineering services to Jim and Paul Luginbuhl, dated May 14, 2000. We previously conducted a radiation survey of the property and presented our findings in a report dated June 7, 2000, Job No. 100 460. A field exploration program consisting of a reconnaissance, exploratory borings and percolation testing was conducted to obtain information on the site and subsurface conditions. Samples of the subsoils obtained during the field exploration were tested in the laboratory to determine their classification, compressibility or swell and other engineering rharacteristics. The results of the field exploration and laboratory testing were analyzed to develop recommendations for project planning and preliminary design. This report summarizes the data obtained during this study and presents our conclusions and recommendations based on the proposed development and subsurface conditions encountered. PROPOSED DEVELOPMENT The 60 acre parcel will be subdivided into 11 lots between 5 and 7 acres in size and located as shown on Fig. 1. The development will consist of single family homes. The building area will generally be in the front part of each lot. A private road will access the building sites from County Road 221. We assume the residences will be typical of the area and be two to three stories with a partial or full basement. The development will be serviced with individual wells and septic disposal systems. If development plans clip ve significantly from those described, we should be notified to re-evaluate the recommendations presented in this report. H -P GEOTECH -2 - SITE CONDITIONS The proposed Native Springs Subdivision is located on the north side of the Colorado River about two miles east of Rifle. The 60 acre property covers parts of the northern half of Section 11 and the southern half of Section 2, T. 5 S., R. 93 W. County Road 221 borders the property on the south and County Road 210 borders the property on the northwest. The Colorado River is located about 3,000 feet to the south and about 50 feet lower in elevation than the property. The general topography in the area is shown by the contour lines on Fig. 1. The ground surface over most of the property slopes down to the southwest at about 2%. Moderately sloping, small alluvial fans are present in the northwestern part of the property. The fan slopes are typically between 5% and 20%. To the northwest of Road 210 the alluvial fan slopes abruptly transition to a very steep terrace escarpment. Slopes on the escarpment average about 80%. Major drainages do not cross through the property. The drainage basins above the alluvial fans are small and restricted to the 160 foot high terrace escarpment. At the time of our study the property was irrigated pasture. Several irrigation ditches are present on the property. GEOLOGIC SETTING The project is located in the Piceance Basin. This regional geologic structure was formed during the Laramide orogeny about 40 to 70 million years ago. In addition to the main basin structure there are other northwest trending secondary folds in this part of the basin (Shrcba and Scott, 1997). The folds have very small amplitudes in this part of the basin and bedding is essentially horizontal. Major faults have not been mapped in the project area. Surficial soil deposits consist of colluvium and alluvium. Formation rock in the area is the Wasatch Formation. FORMATION ROCK Regional geologic mapping shows that formation rock in the project area is the Shire member (Tws) of the Eocene and Paleocene Wasatch Formation (Shroba and Scott, 1997). The rock is covered by surficial soil deposits and outcrops are not I4 -P riPnTPrH • present. It is expected that formation rock is relatively shallow on the terrace escarpment to the northwest of County Road 210, but elsewhere rock is expected to lie well below typical residential foundation depths. The Shire member consists of varied colored claystone, mudstone, and siltstone interbedded with less abundant coarse- grained sandstone (Shroba and Scott, 1997). The claystone, mudstone and siltstone are usually firm but non-cemented. The sandstones are usually cemented and hard. Joints are commonly present in the cemented rock. The beds occur as complex lenses with limited horizontal continuity. SURFICIAL SOIL DEPOSITS The project area is located on a low river terrace (Qtl) that is about 5 to 10 feet above the modern Colorado River channel near the river. At the project site relatively deep upland alluvium (Qua) covers the low river terrace alluvium. River alluvium was enconntered in Borings 1 and 4 at depths of 33 and 45 feet below the ground surface. The river alluvium is a silty to clayey sand and gravel with cobbles. The low river terrace alluvium is in part late Pinedale glacial outwash and younger Holocene river alluvium (Shroba and Scott, 1997). The overlying upland alluvium (Qua) consists of interstratified silt, clay and silty sand. Small alluvial fans (Qaf) cover the upland alluvium in the northwestern part of the property. To the northwest of County Road 210 the alluvial fans transition to shallow colluvium (Qc) on the high terrace escarpment. Bull Lake and older glacial outwash underlies the terrace surfaces at the top of the high escarpment. FIELD EXPLORATION The field exploration for the project was conducted on August 1, 2000. Six exploratory borings were drilled at the locations shown on Pig. 1 to evaluate the subsurface conditions. The borings were advanced with4 inch diameter continuous flight auger powered by a truck -mounted Longyear BK-51HD drill rig. A percolation test hole was drilled next to each boring with a 6 -inch diameter auger. The borings were Iogged by a representative of Hepworth-Pawlak Geotechnical, Inc. N -P f;anrrrw Samples of the subsoils were taken with 1% inch and 2 inch I.D. spoon samplers. The samplers were driven inw the subsoils at various depths with blows from a 140 pound hammer falling 30 inches. This test is similar to the standard penetration test described by ASTM Method D-1586. The penetration resistance values are an indication of the relative density or consistency -of the subsoils. Depths at which the samples were taken and the penetration resistance values are shown on the Logs of Exploratory Borings, Figs. 2 and 3. The samples were returned to our laboratory for review by the project engineer and testing. SUBSURFACE CONDITIONS Graphic logs of the subsurface conditions encountered at the site are shown on Figs. 2 and 3. The subsoils consist of about 11/2 to 2 feet of topsoil overlying stratified sand, silt and clay. The upper soils are slightly moist to moist and medium dense/stiff to wet and soft generally below 5 to 10 feet depth. Dense, silty to clayey sandy gravel and cobbles with boulders was encountered in Borings 1 and 4 at depths of 33 and 45 feet, respectively. Drilling in the dense gravel with auger equipment was difficult due to the cobbles and boulders and drilling refusal was encountered in the deposit. Laboratory testing performed on samples obtained from the borings included natural moisture content and density, finer than sand size gradation analyses and liquid and plastic limits. Results of swell -consolidation testing performed on relatively undisturbed drive samples of the upper soils, presented on Figs. 5 and 6, indicate low to moderate compressibility under conditions of loading and wetting. The samples showed minor settlement/heave potential when wetted under a relatively light constant load. The laboratory testing is summarized in Table I. Free water was typically encountered in the borings at a depth of about 10 feet at the time of drilling. When checked the next day, the borings were dry and had caved at depths of 5 to 10 feet which could be just above the stabilized groundwater level. Boring 3 was dry to the drilled depth of 20 feet. u a ra„rcr„ • -5- GEOLOGIC SITE ASSESSMENT Development of the property as proposed should be feasible based on the geologic conditions with some considerations in the project planning and design. Geologic conditions that should be considered in project planning and design are discussed below. FLOODING AND SURFACE DRAINAGE Large off-site drainage basins are not tributary to the project area. Channels on the alluvial fans in the northwestern part of the site are poorly defined and the fans could be the site of high sediment concentration sheet flooding associated with intense thunderstorms. The flood potential on these fans should be considered by your hydrologist as part of the storm water management and drainage plan for the development. The potential for irrigation ditch blockage and overflow should be included in the hydrologic evaluations. MOISTURE SENSITIVE SOILS The upland alluvium (Qua) encountered in the exploratory borings was wet and soft below a depth of 5 to 10 feet but the upper soil was stiff and relatively dry. It has been our experience that relatively dry soils similar to the upland alluvium (Qua) and alluvial fans (Qat) at the site can be moisture sensitive and experience relatively large settlements if they become wetted after construction. Consideration for residential foundations are discussed in the Preliminary Design Recommendations section of this report. CONSTRUCTION RELATED SLOPE INSTABILITY Slopes in the proposed building envelopes do not exceed about 15%. We do not expect problems with construction related slope instability associated with grading typical of most residential construction in the proposed building envelopes. Grading is not recommended on the steep terrace escarpment to the northwest of County Road 210 unless evaluated by a geotechnical engineer. u D rcn-rcru -6 - EARTHQUAKES The project site could experience moderately strong earthquake ground shaking of Modified Mercalli Intensity VI during a reasonable service life for the development, but the probability for a stronger ground shaking is low. Intensity VI ground shaking is felt by most people and causes general alarm, but results in negligible damage to structures of good design and construction. The occupied structures should be designed to withstand moderately strong ground shaking with little or no damage and not to collapse under stronger ground shaking. The site is located in the Uniform Building Code Seismic Risk Zone 1. Based on our current understanding of the earthquake hazard in this part of Colorado, we see no reason to increase the commonly accepted seismic risk zone of the area. PRE.IMTNARY DESIGN RECOMMENDATIONS The conclusions and recommendations presented below are based on the proposed development, subsurface conditions encountered in the exploratory borings, and our experience in the area. The recommendations are suitable for planning and preliminary design but site specific studies should be conducted for individual lot development. FOUNDATIONS Bearing conditions will probably vary somewhat due to the stratification of the subsoils and the typical shallow groundwater condition. Based on the nature of the proposed construction, shallow spread footings bearing on the upper natural soils should be suitable for building support. We expect the footings can be sized for an allowable bearing pressure in the range of 1,000 psf to 1,500 psf. There could be some potential for additional differential settlement if the bearing soils become wetted. The footing bearing level should be kept relatively shallow to avoid groundwater and soft soil impacts. In general, the footing bearing level should be kept at least 2 feet above the groundwater level. Full basement construction may not be feasible in some areas of the site due to potential shallow groundwater. Foundation walls should be designed to span local anomalies and to resist Iateral earth loadings when acting as retaining structures. H -P GEOTECH -7 - Below grade areas and retaining walls should be protected from wetting and hydrostatic loading by use of an underdrain system. The footings should have a minimum depth of 36 inches for frost protection. FLOOR SLABS Slab -on -grade construction should be feasible for bearing on the natural soils. There could be some potential for settlement/heave if the subsoils become wetted. To reduce the effects of some differential movement, floor slabs should be separated from all bearing walls and columns with expansion joints. Floor slab control joints should be used to reduce damage due to shrinkage cracking. A minimum 4 inch thick layer of free -draining gravel should underlie interior slabs to facilitate drain ge. Floor Levels should be kept at least 2 feet above the groundwater level. UNDERDRAIN SYSTEM Groundwater Ievel was encountered in the exploratory borings at relatively shallow depth and irrigation of the surrounding area will tend to keep the water level shallow. Local perched groundwater can also develop during times of heavy precipitation or seasonal runoff. An nnrlerdrain system should be provided to protect below -grade construction, such as retaining wall and basement areas from wetting and hydrostatic pressure buildup. The drains should consist of drainpipe surrounded above the invert level with free -draining granular material. The drain should be placed at least 1 foot below lowest adjacent finish grade and sloped at a minimum 1% to a suitable gravity outlet or a sump and pump. Shallow crawlspace areas should not need a perimeter foundation urain provided the backfill is well compacted and has a positive slope away from the building. Below grade levels of the buildings should be kept at least 2 feet above the groundwater level. SITE GRADING Cut depths for the building pads should not exceed about 5 to 8 feet depending on the groundwater level. Fills should be limited to about 5 feet deep above existing ground surface. Structural fills should be compacted to at Ieast 95% of the maximum standard Proctor density near optimum moisture content. Prior to fill placement, the H -P GEOTECH -8- subgrade should be carefully prepared by removing all vegetation and topsoil and compacting to at least 90% of standard Proctor density. The on-site soils excluding vegetation and topsoil should be suitable for use in embanlanent fills. The deeper soils may be highly moist and require drying before use as bacb-filt material. SURFACE DRAINAGE The grading plan for the subdivision should consider potential runoff from uphill slopes through the project and at individual sites. Water should not be allowed to pond which could impact slope stability and foundations. To limit infiltration into the bearing soils next to buildings, exterior backfill should be well compacted and have a positive slope away from the building for a distance of 10 feet. Roof downspouts and drains should discharge well beyond the limits of all backfill and landscape irrigation should be restricted. PERCOLATION TESTING Percolation tests were conducted adjacent to each of the exploratory borings to evaluate the feasibility of an infiltration septic disposal systems at the site. The test holes were drilled with 6 inch diameter auger and were soaked with water one day prior to testing. The soils encountered in the percolation holes are similar to those encountered in the exploratory borings shown on Fig. 2 and consist of stratified sand., silt and clay. The percolation test results are presented in Table lI. Based on the subsurface conditions encountered and the percolation test results, conventional infiltration septic disposal systems should be feasible at the site. A mounded system could be needed in shallow groundwater areas. A civil engineer should design the infiltration septic disposal system at the time of each lot development. LINIITATIONS This study has been conducted according to generally accepted geotechnical engineering principles and practices in this area at this time We make no warranty either expressed or implied. The conclusions and recommendations submitted in this H -P GEOTECH -9- repon are based upon the data obtained from the field reconnaissance, review of published geologic reports, the exploratory borings located as shown on Fig. 1, the proposed type of construction and our experience in the area. Our findings include interpolation and extrapolation of the subsurface conditions identified at the exploratory borings and variations in the subsurface conditions may not become evident until excavation is performed. If conditions encountered during construction appear different from those described in this report, we should be notified so that re-evaluation of the recommendations may be made. This report has been prepared for the exclusive use by our client for planning and preliminary design purposes. We are not responsible for technical interpretations by others of our information. As the project evolves, we should provide continued consultation, conduct additional evaluations and review and monitor the implementation of our recommendations. Significant design changes may require additional analysis or modifications to the recommendations presented herein. We recommend on-site observation of excavations and foundation bearing strata and testing of structural fill by a representative of the geotechnical engineer. Respectfully Submitted, HEPWORTH - PAWLAK GEOTECHNICAL, INC. Steven L. Pawlak, P.E. Reviewed by: Daniel E. Hardin, P.E. SLP/rso/ksw cc: Land Design Partners - Attn: Ron Liston H -P GEOTECH -10 - REFERENCES Shroba, R. R., and Scott, R. B., 1997, Geology Map of the Rifle Quadrangle, Garfield County, Colorado: U.S. Geological Survey Open -File Report 97-852. Tweto, 0. and Others, 1978. Geologic Map of the Leadville 1° x 2° Quadrangle, Northwestern Colorado. U.S. Geological Survey Map I-999. H -P GEOTECH • EXPLANATION: Qc - Colluvium Qaf - Alluvial Fan Qua - Upland Alluvium 011- Low River Terrace 0 - 100460 HEPWORTH-PAWLAK GEOTECHNICAL, Inc. Native Springs Subdivision Geology Map and Boring Locations Fill 5 1 ,j J " ,.�/ S// Late ' i - , _Li , ``,tae 1 ' i' 10 B&1 %/QualQtl �E ,,,. ii Lot 11 I 100460 HEPWORTH-PAWLAK GEOTECHNICAL, Inc. Native Springs Subdivision Geology Map and Boring Locations Fill 0 5 10 15 v 90 1 ` a — 0 25 30 35 BORING 1 ELEV.=5371' BORING 2 ELEV =5378' r 20/12 11/12 :ice WC=3.7 �•. DD=100 :'l -200=20 /l r 4/12 WC -29.8 DD=100 -200=98 LL -31 / P1=13 — C'• 4/12 ///r /./5/12 J BORING 3 ELEV.=5386' 20/12 17/12 WC=9.6 DD=115 14/12 10/12 7/12 J 10 15 20 25 30 35 — 40 40 Note: Explanation of symbols is shown on Fig. 4. a CDU - y 0- a) 0 100 450 HEPWORTH - PAWLAK GEOTECHNICAL, INC. LOGS OF EXPLORATORY BORINGS Fig. 2 4 0 W 5 — 10 BORING 4 ELEV.=5389' / 6/12 00=106 —200=64 LL=22 PI=7 4/12 ,-.- 15 / 6/12 90 " 5/12 4 25 30 / 8/12 45 50 CHANGE IN SOIL TYPE AT 45' BORING 5 ELEV.=5360' 5/12 WC -20.3 00=104 —200=66 3/12 3/12 5/12 BORING 6 ELEV.=5374' 15/12 .41 /1 6/12 We=1B.2 00=110 %1 1/4 1/12 3/12 3/12 Note: Explanation of symbols is shown on Fig. 4. 0 5 10 15 20 25 30 45 50 Elevation — Feet 100 460 HEPWORTH - PAWLAK GEOTECHNICAL, INC. LOGS OF EXPLORATORY BORINGS Fig. 3 5 LEGEND: pTOPSOIL; organic sand, silt and clay. SILT AND CLAY (ML—CL); slightly sandy to sandy, stratified, stiff and slightly moist to soft and wet with depth, brown, low plasticity. SAND (SM); silty, sandy silt layers, loose to medium dense, slightly moist to moist, brown, fine to medium sand. pSAND, GRAVEL AND COBBLES (GM—GC); silty, clayey, dense, wet, brown. M 6/12 --s 1 NOTES: Relatively undisturbed drive sample; 2—inch I.D. California liner sample. Drive sample; standard penetration test ( SPT ), 1 3/8—inch I.D. split spoon sample, ASTM D — 1586. Drive sample blow count; indicates that 6 blows of a 140—pound hammer falling 30 inches were required to drive the California or SPT sampler 12 inches. Ground water level at time of drilling. Caved depth when checked on August 2, 2000. Practical drilling refusal. 1. Exploratory borings were drilled on August 1, 2000 with a 4—inch diameter continuous flight power auger. 2. Locations of exploratory borings were measured approximately by pacing from -features shown on the site plan provided. 3. Elevations of exploratory borings were estimated from contours on the site plan provided. 4. The exploratory boring locations and elevations should be considered accurate only to the degree implied by the method used. 5. The lines between materials shown on the exploratory boring logs represent the approximate boundaries between material types and transitions may be gradual. 6. Water level readings shown on the logs were mode at the time and under the conditions indicated. Fluctuation in water level may occur with time. No free water was encountered in Boring 3. 7. Laboratory Testing Results: WC = Water Content ( % ) DD = Dry Density ( pcf ) —200 = Percent passing No. 200 sieve. LL = Liquid Limit ( % ) PI = Plasticity index ( % ) I100 460 HEPWORTH - PAWLAK GEOTECHNICAL, INC. LEGEND AND NOTES Fig. 4 1 Compression Compression — Expansion % 0 1 2 3 4 5 1 D 1 2 3 Moisture Content = 9.0 percent Dry Density = 110 pcf Sample of: Sandy Silt and Clay From: Boring 1 at 2 Feet 0 Compression upon wetting 01 1 0 10 APPLIED PRESSURE — ksf 100 Moisture Content = 9.6 percent Dry Density = 115 pcf Sample of: Sandy Silty Clay From: Boring 3 at 5 Feet Expansion upon wetting 0.1 I100 460 1 0 10 APPLIED PRESSURE — ksf 100 HEPWORTH — PAWLAK GEOTECHNICAL, INC. SWELL—CONSOLIDATION TEST RESULTS Fig. 5 • s 0 1 0 N m 2 E 0 0 3 4 Moisture Content = 18.2 percent Dry Density = 116 pcf Sample of: Sandy Silt and Clay From: Boring 6 at 5 Feet Compression upon wetting i 0.1 1.0 10 APPLIED PRESSURE — ksf 100 100 460 HEPWORTH - PAWLAK GEOTECHNICAL, INC. SWELL -CONSOLIDATION TEST RESULTS Fig. 6 • ', .O 0 0 6 0 U J Q U Z V O c W - o C7Lu, Q Q Q o 7J H z 1— CC 0 a w TEST RESULTS SUMMARY OF S011. On nEDROCI( TYPE Sandy silt and clay ' r CC— N > C/) > m — U > v) Sandy silty day II U J m -- _ v >- o C ti U) _ N ? c m C!) (0 CO U -O m y _ y T -c C ti U) UNCONrINrn COMPRESSIVE STRENGTH (PST} N a CC = 0K z w - G z - I £1 N C I - o E- r CO N N W- N j = Q- 6 - La i z 0 N CO O) I G4 CO CO 0 P a a c q w a* o' NATURAL DRY DENSITY IRcfl o 100 I 100 LO CO 0 104 I o NATURAL MOISTURE CONTENT 1%I o 07 h CO. N [o Q) C) co ' 20.3 11 N 2 SAMPLE LOCATION DEPTH Ileetl 2 5 10 L() 5 l2) L7 0 e 0 m r- N CO d' LO 0 HEPWORTH-PAWLA}C GEOTECHNICAL, INC. TABLE II PERCOLATION TEST RESULTS JOB NO.100 460 PAGE 1 OF 2 HOLE NO. HOLE DEPTH (INCHES) LENGTH OF INTERVAL (MINI WATER DEPTH AT START OF INTERVAL (INCHES) WATER DEPTH AT END OF INTERVAL (INCHES) DROP IN WATER LEVEL (INCHES) AVERAGE PERCOLATION RATE (MIN./INCHI P-1 48 20 37 36 1 40 36 351/2 1/2 351/2 35 112 P-2 46 5 18 1/2 15 1/2 3 3 15 1/2 14 1 1/2 14 12 2 12 101/2 11/2 101/2 81/2_ 2 P-3 50 5 28 27 1/2 112 10 27 1/2 27 112 27 26 1/2 112 26 1/2 26 1/2 P-4 51 10 30 26 4 5 26 24 2 24 22 2 22 20 2 20 18 2 Note: Tests were conducted in 6 -inch diameter auger holes on August 2, 2000. The holes were drilled and soaked on August 1, 2000. The percolation holes were drilled next to the corresponding numbered boring (see Fig. 1). • h .w HEPWORTH-PAWLAK GEOTECHNICAL, INC. TABLE 11 PERCOLATION TEST RESULTS JOB NO. 100 460 PAGE 2 OF 2 HOLE NO. HOLE DEPTH (INCHES) LENGTH DF INTERVAL (MIN) WATER DEPTH AT START OF INTERVAL (INCHES) WATER DEPTH AT END OF INTERVAL (INCHES) DROP IN WATER LEVEL (INCHES) AVERAGE PERCOLATION RATE (MIN./INCH) P-5 46 5 refill 141/2 , 12 21/2 2 25 21 4 21 17 4 17 131/2 31/2 P-6 59 20 36112 351/2 1 20 35 1/2 34 1/2 1 34 1/2 33 112 1 Note: Tests were conducted in 6 -inch diameter auger holes on August 2, 2000. The holes were drilled and soaked on August 1, 2000. The percolation holes were drilled next to the corresponding numbered boring (see Fig. 1). CIVIL ENGINEERING May 31, 2005 Garfield County Building and Planning 108 W. 8th Street Glenwood Springs, CO 81601 An EmployccOwncd Company Re: Lot 10 -Native Springs Subdivision HCE Project Number 2041033.00 x 0218 To Mark Bean: LAND SURVEYING The following letter is to confirm the engineer's inspection of the revised septic system for Lot 10 of the Native Springs Subdivision. High Country Engineering's field inspector performed the field inspections. The design included a 1,000 gallon septic tank and an absorption field consisting of 31 infiltrator units configured in 2 rows of 10 and 1 row of 11 units in a trench system. The infiltrator trenches were slightly reconfigured and moved approximate 35 -feet southwest from the design location_ The house line, effluent line, and manifold piping were adjusted accordingly. The contractor will backfill the system and will provide positive drainage away from the field. Including the minor change, the system has been constructed with the intent of the plans and specifications. If you have any questions, or need additional information, please contact us. Sincerely, HIGH COUNTRY ENGINEERIN 1517 Blake Avenue, Suite 101 Glenwood Springs, CO 81601 970.945.8676 phone 970.945.2555 fax www.hceng.com 14 Inverness Drive East, Suite F-120 Englewood, CO 80112 303.925.0544 phone 303.925.0547 fax SECTIONS 2 &11. TOWNSHIP 6 S, RANCE 93 W, 6TH P.M. VICINITY MAP SCALE ,• . 2000' CORD DRAWING MAY 31, 2005 RFIELD COUNTY )S PERMIT #4012