HomeMy WebLinkAbout1.0 ApplicationPursusant to C
amended, and the
adopted April 23,
of County Commissioners of Garfielcl
Resolution rhe division "r Va {(u.,
I]EPORE THE BOARD OP COUNTY COI,lMISSIONER.S OF
G.\RP I ELD COUNTY , COLORADO
PETITION FOR EXEMPTION
.R.S. (197J) Secrion J0_28_t0t (10) (a) _ (
Subdivision Regulations of Garfield County,
1984 Section 2220.49, the untlersigneJ
respectfully petitions the goard
d) as
Colorado,
Co,unty, CoIorado, to exempt by
e tract of land i*o_ X'Z- tractsp1t,UJ;*6,#ugtr'lf Lt t-*;&-tt l^ll{., .6|{-{ u? t,1" kt rc.' o !, rk "," w6:,#i ^!r-& G i,J?;{d
6nPloximatelyl
I t , t. n n tl ,'t , -t L- -*-
appr o x ima L:tv!@_6!)l!{...6,ffiu"dff ,Lokt'f€.:orc, tK, ,hTfti#!/#-#r Giffi;{d'"'/bft iwNs*4^1fe.#ffytl"f f;;{*#rn. rerms are used and crerined in
of
/"t/./of
c'R's' (1973) section 3o-28-101 (10) (a) - (d) and the Garfierd counrysubdivision Regulations for the reasons stated bel0w:
t,
SUBMITTAL RCQUIREMENTS :
StmBItrlH#:;:;i:;s rhe review crireria musr be submirred wirh
4.
4.
D.
sketch maD at a minimum scale of r " =200 ' showing the I egaldescription of tlu -JioJ".av,
dirnension and area of ar1 rors orseparate inreresrs to be ';.;;;;;;^ access to a publ icfigft-of-wayr dDd any proposed easemerts for drainage,rlrlgationr dccess or utifitiu"; - --
vicinity map ab a minimum scale of 1"-2000, showing Ihe generaltopographic and geogrupni" reration of !lru propg-sed exemption to5:: ;:5:";l::l:"ni:";.otiil';""ili;i, i'"i r "",' i;l",n', "n u' "opy ;;Copy of the Oegd sfrowing-ot\,nership by the applicant, or a letterf rom the proper ty ornu. ii ) if o*-,ei ;1"; rhe appl i.canr; andNames ancl addrLs"u" of -o*nu." of recorrl or" ii,iJ . imnetliatelyadjoining and wiLhin ioo-t::L-oi-tr,;-;;oposed exempr,ron, mineralowners and lessees of minerar" o*nu.i-oF-.ecord of th; property to::nr"."Xi3li"3;u "no t;;;;t" or u"r- srrucrure proposeci ror
Evidence of tf," soil types and characteristics of each type; andProof of legal-and aoeqLu[" source of domestic water for each 1otcreared, merhod of sewise aisposir,- ;;; -i;;tll'"lr
approvar. of'f ire protection pran rr6m appropr iate rire district; a,clrf connecrion to u "o**unitv ;;-;;;icipar watei oi sewer sysrem,},irr?;;:llSoi" l".ia:a;;--;."; tr,"-"g",i*.ni,rg ;";y sra rins aNarrative explaining',"hy exemption is being requested; andrt sharr be demons[.ufia -Lr,uL !h; ;;, ""r .6xisi;;-;;-c]escr ibed onJanuary 1, 1973. or urru farcet as it "rists presenLry is one of
!iir!!5"":n31",::;.i, fi;:it" "'"utuJ i'on' a ia,g*i-parcer as j rA $100'00 fee must be submitted with the apprication.
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Telephone Number
EXEMPTI ON
APPLICABILITY
The Board of County Commissioners has the discretionary power Io exempE adivision of land from the definition of subdivision and thereuy from theprocedure in these Regulations, provided the Board determines that suchexemption will not irnpair or defeat the stated purpose of the subdivisionRegulations nor be detrimental to Ehe general puUlic welfare. The Boardshall make exenption decisions in accorclance vrith the requirements ofthese regulatj.ons. Following a review of the individual facts of eachapplication in light of the requirements of these Regulatior:s, the Boardmay aPprove, conditionally approve or deny an exemption. An appli.cationf9. exemption must satisfy, at a minirlumr afi of Ehe review criLeria
1 isted below. Compl iance with the review cr iter ia, however , does rlotensure exemption. The Board also may consider additonal factors lisLecl inSection B:60 of the Subdivision negulations.
A. No more than a total of four (4) lotsr pdrcels, interests or ilwellipgunits will be created from any parcel, a! that parcel was described i;Ehe records of the Garfield County Clert< anA Recorder,s Office onJanuary 1,1973r and is not a patt of a recorded subdivision; however,any Parcel to be divided by exempbion that is spl it by a publicrighE-of-way (sLate or Federal highway, county road or railroad) ornatural feature, preventing joint use of the propose<1 tracts, and thecivision occurs along the public right-of-way or natural feature, such' parcels thereby created hdy, ar [fre discretion of the Boarci, not beconsidered to have been created by exemption wibh regard to the four(4) 1ot, parcel, interest or dwellin,j unit limitation obherwiseappl i cabl e;B. A11 Garfield county zoning reguirements will be met; andC. A11 lots created will have 1ega1 access to a public right-of-way andany necessary access easements have been obEained or are i; theprocess of being obtained; andD. Provision has been made for an adequate source of -water in terms ofboth the 1ega1 and pttysicll guality, quantity and depepciability, and asuitable tyPe of sewage disposal to serve each proposed lot; anaE ' All state and 1ocal environmental hea] Lh ancj saiety requirements havebeen met or are in the process of being met; andr" Provision has been made for any r"quired road or storm clrainageimpr ov.ements ,. a ndG. Fire protecEion has been approved by the appropriaEe fire district.
H ' Any necessary dra inage, ir r igation or utir itv easements have beenobtained or are in the process or being obtainet; andr. school fees, taxes bnd special assessments have been paid.(The School ImpacE Fee is $200.00 for each new lot created).
PROCEDURES
A.
B.
A request for exemption sha1l be submitted to
P{oyided by the Garfield County Deparrment ofDivision. Two (Z) copies of the apblicaEion,information sha1l be submitted
the Board on forms
Developmen L/planning
maps and supplemental
The - Planning Division shal1 review the exemption request forcompleteness wi!!,in eight (B) days of submittal. rf ilcompfete, Iheappl ication shall be withtirawn from consideration and Ehe appl icantnotified of the additional information neecled. If the appl iciLion iscomplete, the applicant sha11 be notified in writing of- tfre time andplace of Ehe Board of County Commissioners meeIing at whicS 15erequest shall be considered. In either caser notification shall occurwithin fifteen ( 15 ) days of submirtal.
c.Notice of the public meeting shall be maired by certifie<l mailr r€turnreceipt requested, to owners of record of fana immecliately adjoiningand within 200 feet of the proposed exemption, to minerar owners andlessees of mineral owners of record of Ehe Iand proposed forexemption, and to tenants of any "tircture proposed for conversion.The exetnption site sha1l be poste- clearly antl conspicuousry visiblefrom a public-righ!-of-way wirr, noria;-;igns provi;;;' by rhe planninsDivision ' A11 notices srrirl be maired at least f if t,een (15 ) anil notmore than thirt'y- ( 30 ) days pr ior to the meebing. The applicant sharlbe responsible for maiiing the notices ana sharl prese.t proof ofmailing at the meeting.
At or within fifteen ( r5) days of the meeting, the Board shaIlapprove, conditionarly approve or cleny the exemption reguest. Thereasons for denial or any-tonditions oi--upp.oval snirl be set forEh inttle minutes of the meeting or in a written resolution. An applicantdenied exemption shall -fol1ow th; suuaivision procedure in theseRegulations.
D.
$xre
Z,,T*N
August 12, 7987
The Pl ann'ing Department
Garfiel d County
109 8th Street, Su'ite 303
Glenwood Springs, Co. 8160i
Gentl emen:
The Colorado National Bank of Denver as Trustee for the Estate of Henry
P. t,Jilliams, is the owner of approximately 19 acres located in Sections
35 and 36 located Nt,J of the Canyon Creek interchange and also a small
parcel located Shl of the interchange.
Please consider th'is letter as your authority to deal w'ith Greg McKennis
on our behalf in matters pertaining to zoning and Senate B'ill 35 exemptions.
If furthe; specific authorization js needed, please let me know.
COLOh^DO NAtrlONAL BANK
OF DENVER
'iFil,",,sYours
Homer L. Hancock
V'ice President
HLH: kr
Seventeenth Street at Champa
Denver, Colorado 80202
(303) 893-1862
Mailing Address:
P.O. Box 5168
Denver, CO 802'17
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tTu,l:1, h1.I"r',r selr ra.i coj)vev to r{psFJ p. i.TLLiijl.S, .;F.. cf the ,-.ffi
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Pr"s "ott lt. *t center o! alddLe of carnon creek as tt nov ls sltuatc i;ittsod.as1jertar:ri1ngaouthacro5stheCcIorr.r]<lILlver1to-r"{|3
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aatd o11 and llnerjs.
1"":,ot' in*L prrrt rf t'e fououir.rg cescrlbed rots a'a parcela of,
r3^ng no.rth.of the center r'ne of lhe colorecio R[.verr. to-n!.tr '.
' :t* - Nt/>6E,'ltt'o ncrth "r[(;r; ?t ,n" souureast cuarferJand ths ";ffit'rf '
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t,Jr Pc;ter Hatt,ivii Ur;qt1=r r-lth uil <i.ii,:h ;rir,l itl,ch rlshts,
veter and vi.ter rLgrt s u.leC o:r or lrt ccnnecticc vtbh seld
lrind.n u..d prrrllr:'r.ia,rly en r:::tdlyl.rlerl c,tt+-nr.]i ili,crest Lr rudto r.irs Cnrurorr ;lro*k Dltcn, 'Loyether r.,ltlr cuo-hrl.i' o.f ti.c uaEer
edjuilicateu to esi(: ditc} by thu cecr,-a of rl^.e 0j.s+.rtc! Court
.!-ll and for salC C+rrfielri Cor.mtT ,rrr.Lei't:q l(a7 )I, 1809, for
\ist"€r Dlstrlct No. Jl, rtutd dttch trrlnr nurh'rr,:.i dl, 'rtth
?rlcrlty Ho. JE, Llra vat*r' ttrorebT tlocroul bvin; e.na.erd cno-
lrrrlf cublc f':'et psr oecond ot' t,tic^:, r'o:e.opt!-ng arrd rueerrlngfrrn tbo aborra landa aI] of bhat porttol of thr northeast quattrr
of 'Lhe aoutheast quarter of S.rct-!"on J5, Tor.n 5 Sor.rth, Renge 90yect, 6th P.H. locatetl ar.d altrraLed norah of tho nor*.-tr'ILrs or'
thc right of vay of the Dsnver u:d i'Llo Cra::cig ltallroad.
. Coipremclng at tha souLhoasL comur nr.-bu. I frca uirlch tha
eenter of SecL[on )5, Tom 5 South, Ilange 90'Jast, 6tlr P.H.
e.s. eatabllshed by Briidt 1r. about 16$3, bel.ng s,:rrth l! dogrees,
.(5 alnutes €ast -?84.1 foet; thsn':o soutli 82 <iagreae 15 ilnutes
vest 40.8 feet Lo corncr nunber 21 fhence northJO.dogroea .
.1,5 alnuLee Hest 136.6 feet to cornei" nrr:iber 3r locat,ed on thc' ssuLh bsrlk of thE Tlbbetts Dttch fr.on vhls\ corner a'cottoavoo,i
tre€ blazed \rith X s.ark and nnllad tn ttie ccn',,er of tht I nark-.
beLng oorth 2( dagreee 4,5 ufurutes vest 6.5 fcct; thenco north
65 degreaa 45 ntnutes easl {,!i.-) fot't to corner nuabor 4localedon Lhu south'banks of thr TlbbeLt,s Ditch a.,nrl i.ro.l the.:cs routh.
? .legrees L5 ntlnutes eest i-/+8,6 r'eslt Lo ccnrer beto.g .the potnt
ol' cegknlng.
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ALl of ttrat tra,ct of land sltuatc Ln the souLheast Srortton of
the souttroast gusr+.:r of ttra norLhrss; o.ua.rter, liectio.l lir Tovn
J;o.,:uth, I!,rrnge 9O Uust,, oth P,;{. enrl Ccsrrr'ltod as i}'i.ng south
., cf li.6 gar:nty tr:trl end no:-t,h cf ii:u r'!.ght,,-.f r'-\y cf the Denv*r
:l:.C Ii!o Orairo.g !i:sLet'tr F:i.'.l,rcir:i, Ltie.ra>t,l;l to.ur.!aiy cf vhJ.ci'r
e0:U:c!'Jes uir.L tr,e Fari,;ri:I i;(rtul'Jt^I',v llnu .li' j:" 1.2 rlc'.tLt4ta,ut
qusr-ter of Lho nuruhh'rrsL qulrter, S,rcftorr J5r.bs!r.g trlar:Erlir
ln shape s-nd ccelprislng afJpr,)xLc,e;el;' tvo e--,C c{rs-helf acras-
fnere ls er.ceptrxi ald tEsar.re.l irop the e.boye '"he foiloving:
Propert;r cioscrlbed In Docr,ngnt llo. ilf!9j of P.ecords tn Bool
159 at pagx fi of tho I'l:rcorCs In Lhe Oft'lce of the Cicrt trs'l
Bccorder of Oarfleld Corrnty, Colorado, t"o vhich rsfcruee ,.s
uaCe for aonB ccclpletc Ccacriptlcn, anti progerty dcscrlb€d 1rr
Dosurent No. 1.041?2 In Book 16i at ps-gd37l of s,foraEald Recordsr
to vhlch "ofuEiE-ts nada for uora cooplete descrlptlon. Also
prop€rty dencrlbcd lrr Doq:nents Noo. Il8Ua and ll,8l99 rocordod.:. ln aforesatd fi,ecords, to uhlch iefcrencc ls nade for uor'o co-
plete doscrlptlon.
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U . S . II i Slrtalt '' !,'lo 'P.oad ,'ontarining
ii;,,iiri [li[li]ei--rfi-.,g so.,,Lh and ltaEt o{ the risl"rt of vtav
, , of the gohuul-r-Rio Grande i'lesteln Fai-Iro.rd;
l',lr"o exceptins at.r that pal-t o{ ll'" :I-}41-I1-}/4
, di-Jui6-si"lj.i"-"rs rrorthtr:i.y of ure Prerrc'terga6t
, Dl{:r:h as descrlbed j-n l'larr:a:rt1' I)cred recorded,in3i*if;'I."EIJiiiuli l-"-'jiiioi't:' I"':1_'::":t:*. :t$I'lltH.I=ii'ii"-ci"''[ ana nlco'S?:.?l ?:'I*']d'.i-oo".,trent lio- 1I8144 i'n Book
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: :i,1i.1,,1 ,,,,,,,: A16tr alt,thAt parL of the SE I,/{ t{l'l 1/4 of --SectlOn
",,i.!,.:,,, '3s-lylil foiti,Ltry of the r:!ght cf wa'r of u' s''
' :,,:.i.... . uigry'ralu*tl'i'i"ti'o Ii"tn a'i East or tle countv
,ill'',r
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' I AIso, all thet part of the N I/2 sE 1/A: {E -L/A'sn ll4-;d-srl f7a :'iil l.i4-of sjcct-ian 35 lving
Norrh"rfi-ot tr," "er.,r"i ri,,. oi the colorado River;
i. r,x."eiini if f o1r- anil niner;ris contsaine'rJ wlthin
.:,.: ,,.,'..,1 ftf teen acres of }and si..uate i:r thc Norti-reast
ilil;;'#-$t; itia slt r/4 Ne I/4 as reserved in
tlitliti:D*;; iecotata in rhe' ofrice of the crerk'
lft^;;Atil;;; Garfierci cou::tv, colora<lo-as
rlocunent !io. lilii- ii ]looi: f f i'it-Page 516 thercof i
thcreof;
# "uo*rent'
or- rtghti:,
":: county, colo:-adc'
L79 a.t'Page 177
trlr.o exccptiBg all tlrat Fltl- "i.:l?.-tol"{l-t:.:{ili" ;JiTiltfi"*ii i,i"i''l.r N cr t t' c'l1' ?-r. ^*e - 1lsh u
;; ;;*";"il;-;.Ii'ui i nio GI1':i=- l'11":*: :'dcscri.bed J-n $t;;;;;i'v-Deed !'ecordcd - lt-!l:-:f fisf*"tiri.ii v- p""J ie "';rc cd
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i." ^!l:-:f f ieedcscrr.DeG ,.n narr'rItL'y vEE\r '-* ^' : ;;:,I- ^^..-.*.,
r .o, Lhe clerle ana Rec-ordel of Gar:fi:r9.c?:tjt{i ,,.,,:?"ff1"8i"';il '#;'i;;';;;"oi car:rierd countvr ' -
Colorado, as Docuxqent No' 68809 :'n sook 123, at 'j''i'i'iaq* 16?., tlrereofl '
,PaEe
&}so o(*epting roacl rights 9f riay heretofore convcyed
' to ttrc ;SQard of ' E;;;y=a;n'c. :i ss i o'ne rs of Ga rf le ld
county'ii,'Coloraio-by lJi5r""ty. n"i:at rqcorcled tn ;:''''
the offLce of itJtr"ir-a''a' R:cou!:L?f .:"I:r.3ra
ffirffil;hF*:,m* :l; :3' "3:r':"1"#'tr2,6ziin. gsoh,fig rrt Fago 3?7 therec'f ; "'i',,1'
,1;;rl;[1 yr,11 '] ' i. l:.': i , I
o eorcepting a 100 foo: railroad ri-ght "f ::l' *
ve,vad to the D";;";-s Rio Gran<te tl6stern !1l1::ud;###}"iloi ;;";a;a -il t!:.-"rllfl*?i*,i,:
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LP. ZANCANELLA, ChIef
JAMES MASON, Agst. Chlef
MARTIN ZEMLOCK Captaln
P. PAYNE, Secy. Treaa.
JAMES BIINCO, Lleut.
JACK JONES, Lleut.
Glenwood Springs Fire f)epartment
Member of Colorado State Firemen's Assoclation
806 Cooper
GLENWOOD SPRINGS, COLORADO 81 601
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atrle^waier capacity is modcrate. Effective rooting depthis 60 inches. Surface runoff is medium, and the irosionhazard is moderate.
The Pena soil is deep and welt drained. Typicaily, thesurface layer is about 12 inches thick. The upper part ofthe surface layer is dark grayish brown stony'loam, andthe lower part is dark grayiih brown very stony loam.The substratum is yery. pite brown very stony sandyloam to a depth of 60 inches.
. . Permeability of the pena soil is moderate, and availa_ble. water capacity is low. Effective rooting depth is 60inches. Runoff is slow, and the erosion hazard is moder_ate.
lncluded with these soils in mapping are small areas ofOlney and potts soits rhat nave'irofei ot o to p i;_cent. These areas are on small, isolated mesas and,*g ,p 5 to 10 percent of the complex.
.. Tt ig complex is used mainty for witdtife habitat andlimited grazing.
...ft- !?!ir" vegeration is mainty needleandrhread,wneatgrasses, mountainmahogany, and sagebrush.. When range condition detelriorates, forbs and shrubsincrease. Properly managing grazing'maintains and im_proves range condition. When the rahge is in poor condi-tion,. seeding is practical. Areas must 6e careiutty seteci-ed to avoid the concentration of stones. pubescenl
,,r., ilt', i,:"i,; i.,oli li. L,iUWtt gtly;, try :,irii,;) , .r:t, cil,UUr. i
rnches thick. The substratum rs sand, cobbles, and
gravel to a depth of 60 inches.
Permeability of the Atencio soil is moderate, and avail-
able water capacity is low. Effective rooting depth is 60
inches or more. Surface runoff is slow, and the erosion
hazard is slight.
The Azeltine soil is deep and well drained. Typically,
the surface layer is reddish gray gravelly sandy loam
about 8 inches thick. The underlying layer is reddish
brown gravelly sandy loam about 10 inches thick. The
substratum is calcareous sand, gravel, and cobbles to a
depth of 60 inches or more.
Permeability of the Azeltine soil is moderately rapid,
and water capacity is very low. Effective rooting depth is
about 60 inches or more. Surface runofl is slow, and the
erosion hazard is slight.
These soils are used mainly for grazing and crops.
Alfalfa, small grains, potatoes, and grass-legume hay are
the main crops.
This soil is irrigated mainly by flooding. Grassed water-
ways and minimum tillage prevent serious erosion. Cover
crops or stubble mulching in dryfarmed areas also
reduce erosion.
The native vegetation on these soils is mainly wheat-
grass, sagebrush, and needleandthread.
When range condition deteriorates, forbs and shrubs
increase. When the range is in poor condition, undesira-
ble weeds and annual plants are numerous. Properly
managing grazing maintains and improves range condi-
tion. Seeding improves range in poor condition. Crested
wheatgrass, western wheatgrass, and Russian wildrye
are suitable for seeding. Preparing a seedbed and drilling
the seed are good practices. Reducing brush improves
the range.
Pheasant, dove, rabbit, squirrel, and some deer find
food and shelter on these soils, mainly in areas of crops.
Use of this soil for community development or as a
source of construction material is limited by the large
stones. Special design is needed for septic tank absorp-
tion fields because of seepage and the possibility of
polluting ground water.
This complex is in capability subclass lVs, irrigated,
and Vls, nonirrigated.
9-Badland. This broadly defined unit consists of
steep and very steep, nearly barren land dissected by
many intermittent drainage channels that have cut into
the soft shale and sandstone of the Green River Forma-
tion and into the soft shale and siltstone of the Wasatch,
Mancos, and Mesa Verde Formations. Badland occurs
throughout the survey area, mainly on steep foothills and
mountainsides that have outcrops of shale or sandstone.
_ About 85 percent or more of the area is unvegetated.
The water erosion hazard is very severe, and erosion is
active.
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wheatgrass,weStern-wheatgrass,anonij-ui,"g'.;;-;;;
::libl:-l"r_1"jins. preparing a see_dbed"an;;?ittino rh; :seed a.re good practices. Controlling brush irfr-or"sareas .that are producing more wooO! shrubs than arenormally found in the potential plant community, but con-trolling brush may damage deei habitat.
.Cottontail rabbit, squirrel, pheasant, mourning dove,wird turkey, and some mure deer find habitat oi trls"soils.
Qo-mmunity development is limited by the steep slopesand frost action in the Ascalon soil and by .t""p iiop".and stones in the pena soil.
This complex is in capability subctass Vle, nonirrigated.
8-Atenclo-Azelflne complex, 1 to 3 percentslopes. These nearly level to genity sloping soifJ are onalluvial fans and terraces. Elevition'ranges Irom 5,000 i;7,000 feet. The soits formed in mixed altuvium lLiir"ifrom red-bed shale and sandstone. The average annualprecipitation is about 14 inches, the average annuar airlemperature is about.47 degrees F, and"the il;d;annual froshfree period is about 110 davs.The Atencio soil makes up about +'S'p"r"ent of themap unit, and the Azeltine soil makes up'about 45 p*cent. Exposed areas of gravel mat<e up ,6ort f O percentof the unit.
The Atencio soil is {eep and well drained. Typicalty,the surface layer is dark reddisn gray ."ioy loam about11 inches thick. The upper part oi tne suUsoit is reddishbrown graveily sandy ciay ioam "Uort-ii inches thick,
90
la
IV
TT
66-Torriorthents-Camborthids-Rock outcrop com-
plex, steep. This broadly defined unit consists of ex-
posed sandstone and shale bedrock, loose stones, and
soils that are shallow to deep over sandstone and shale
bedrock and stony basaltic alluvium. This complex
occurs throughout the survey area. The soils and out-
crops are moderately steep to very steep. Slope ranges
from 15 to 70 percent.
Torriorthents make up about 45 percent of the com-
plex, Camborthids make up 20 percent, and Rock out-
crop makes up 15 percent. The Torriorthents are on
foothills and mountainsides below Rock outcrop. The
moderately steep Camborthids are on lower toe slopes
and concave open areas on foothills and mountainsides.
Torriorthents are shallow to moderately deep. They
are generally clayey to loamy and contain variable
amounts of gravel, cobbles, and stones. The surface is
normally covered with stones weathered from the higher-
lying Rock outcrop. South of the Colorado River, basaltic
stones and cobbles are on the surface.
Camborthids are shallow to deep. They are generally
clayey to loamy and have slightly more clay in the sub-
soil than in the surface layer. The surface layer is light
colored. The profile is normally free of stones, but scat-
tered basalt stones, cobbles, and sandstone fragments
are on the surface.
The Rock outcrop is mainly Mesa Verde sandstone
and Wasatch shale. Some areas are covered with basal-
tic boulders and stones. Small areas of limestone out-
crops and exposed gypsum are in the eastern part of the
survey area.
lncluded in mapping are small, isolated areas of llde-
fonso, Lazea(, Ansari, Begay, Heldt, and Dollard soils.
These intermlttent areas make up 10 to 20 percent of
this map unit.
This complex is used for grazing, wildlife habitat, and
recreation.
The stones on the surface and the steep slopes make
this complex unsuitable for crops. Some areas can be
reseeded to pasture by broadcast seeding. Other plant-
ing methods are made difficult by the stones and slopes.
The native vegetation includes wheatgrasses, blue-
grasses, lndian ricegrass, needlegrasses, bitterbrush,
mountainmahogany, sagebrush, and an overstory of
pinyon and juniper.
The value of grazing is fair. The vegetation should be
managed to maintain wood production and limited graz-
ing. Selectively thinning the pinyon and juniper improves
grazing and provides firewood and posts. Steep slopes,
moderate to severe erosion hazard, and slow regrowth
of trees aflect harvesting and management.
. Most of this complex is a prime wintering area for
oeer. Rabbits, coyote, and a few elk also find food and
cover on this complex.
_ Building is limited by steep slopes and stoniness.lhese limitations can be overcome by appropriate
design and construction.
This complex is in capability subclass Vlle, nonirrigat-
ed.
67-Torriorthents-Rock outcrop complex, steep.
This broadly defined unit consists of exposed sandstone
and shale bedrock and stony soils that are shallow to
moderately deep over sandstone and shale and stony
basaltic alluvium. Areas of this complex occur throughout
the survey area. The soils and outcrops are moderately
steep to very steep. Slope ranges from 15 to 70 percent.
Torriorthents make up about 60 percent of this com-
plex, and Rock outcrop makes up 25 percent. The Tor-
riorthents are on foothills and mountainsides below the
Rock outcrop.
Torriorthents are generally clayey to loamy and con-
tain variable amounts of gravel, cobbles, and stones.
The surface is normally covered with stones weathered
from the higher-lying Rock outcrop. South of the Colora-
do River, stones and cobbles of basalt ar€ on the sur-
face.
The Rock outcrop is mainly Mesa Verde sandstone
and Wasatch shale. Some areas are covered with basal-
tic boulders and stones. Small areas of limestone out-
crops and exposed gypsum are in the eastern part of the
survey area.
lncluded in mapping are small isolated areas of llde-
fonso, Lazear, Ansari, Gaynor, Tridell, and Nihill soils.
These intermittent areas make up 10 to 15 percent of
this map unit.
This complex is used for limited grazing, wildlife habi-
tat, and recreation.
Because of the stones on the surface, the Rock out-
crop, and the steep slope, this complex is unsuited to
crops.
The native vegetation includes wheatgrass, bluegrass,
lndian ricegrass, needlegrass, bitterbrush, sagebrush,
mountainmahogany and an overstory of pinyon and juni-
per.
The vegetation should be managed to maintain wood
production and limited grazing. Selectively thinning the
pinyon and juniper improves grazing and provides fire-
wood and posts. Steep slopes, moderate to severe ero-
sion hazard, and slow regrowth of trees affect harvesting
and management.
Most of this complex is a prime wintering area for
deer. Rabbits, coyole, and a few elk also find food and
cover on this complex.
Community development is limited by the Rock out-
crop, steep slopes, and stoniness. These limitations can
be overcome by appropriate design and construction.
This complex is in capability subclass Vlle, nonirrigat-
ed.
68-Vale silt loam, 3 to 6 percent slopes. This deep,
well drained, gently sloping soil is on mesas, terraces,
and alluvial fans. Elevation ranges from 5,000 to 7,200
feet. This soil formed in calcareous eolian material. The
38
average annual precipitation is about 14 inches, the
average annual air temperature is about 48 degrees F,
and the average frost-free period is about 120 days.
Typically, the surface layer is brown silt loam about 7
inches thick. The subsoil is brown silt loam and silty clay
loam about 19 inches thick. The substratum is pink silt
loam to a depth of 60 inches.
lncluded with this soil in mapping are small areas of
Morval soils that have slopes of 3 to 6 percent. These
areas make up 5 to 10 percent of the map unit.
Permeability is moderate, and available water capacity
is high. Effective rooting depth is more than 60 inches.
Surface runoff is medium, and the erosion hazard is
moderate.
This soil is used mainly for irrigated crops and hay.
Small grains, corn, potatoes, alfalfa, and grass hay are
grown. Small areas are used for grazing.
This soil is usually irrigated by flooding, but furrows or
sprinklers are also used.
The native vegetation on this soil is mainly need-
leandthread, wheatgrass, muttongrass, and sagebrush.
When range condition deteriorates, forbs and shrubs
increase. When the range is in poor condition, undesira-
ble weeds and annual plants are numerous. Properly
managing grazing maintains and improves range condi-
tion. Reducing brush improves the range. Seeding im-
proves range in poor condition. Pubescent wheatgrass,
western wheatgrass, and big bluegrass are suitable for
seeding. Preparing a seedbed and drilling the seed are
good practices.
Cottontail rabbit, mourning dove, wild turkey, and mule
deer find habitat on this soil.
Community development and recreation are limited by
low strength and clayey texture. Roads, ditches, and
building foundations can be designed to compensate for
these limitations.
This soil is in capability subclass llle, irrigated and
nonirrigated.
69-Vale sitt loam, 6 to 12 percent slopes. This
deep, well drained, moderately sloping to rolling soil is
on mesas, benches, and alluvial fans. Elevation ranges
from 5,000 lo 7,200 feet. This soil formed in calcareous
eolian material. The average annual precipitation is about
14 inches, the average annual air temperature is about
48 degrees F, and average frost-free period is about 120
days.
Typically, the surface layer is brown silt loam about 7
inches thick. The subsoil is brown silt loam and silty clay
loam about 19 inches thick. The substratum is pink silt
loam to a depth of 60 inches.
lncluded with this soil in mapptng are small areas of
Morval soils that have slopes of 6 to 12 percent. These
areas make uo 5 to 10 percent of the map unit.
a) -,,rir,-.1liitir,,, r. , i ,, rt-, i..,1 -, lilrrrl:r ,.11i ,. t.: , i\/
SOIL SURVEY
Surface runoff is medium, and the erosion hazard is
moderate.
This soil is used mainly for irrigated crops and hay.
Small grains, corn, potatoes, alfalfa, and grass hay are
grown. Some areas are used for grazing.
This soil is usually inigated by flooding, but furrows or
sprinklers are also used.
The native vegetation on this soil is mainly need-
leandthread, wheatgrass, muttongrass, and sagebrush.
When range condition deteriorates, forbs and shrubs
increase. When the range is in poor condition, undesira-
ble weeds and annual plants are numerous. Properly
managing grazing maintains and improves range condi-
tion. Reducing brush improves the range. Seeding im-
proves range in p.oor condition. Pubescent wheatgrass,
western wheatgrass, and big bluegrass are suitable for
seeding. Preparing a seedbed and drilling the seed are
good practices.
Cottontail rabbit, mourning dove, wild turkey, and mule
deer find habitat on this soil.
Community development and recreation are limited by
low strength, clayey texture, and slope. Roads, ditches,
and building foundations can be designed to compen-
sate for these limitations.
This soil is in capability subclass lVe, irrigated and
nonirrigated.
70-Vale silt loam, 12 lo 25 percent slopes. This
deep, well drained, strongly sloping to hilly soil is on
mesas, mesa sides, and alluvial fans. Elevation ranges
from 5,000 lo 7,200 feet. This soil formed in calcareous
eolian material. The average annual precipitation is about
14 inches, the average annual air temperature is about
48 degrees F, and the average frost-free period is about
120 days.
Typically, the surface layer is brown silt loam about 7
inches thick. The subsoil is brown silt loam and silty clay
loam about 'lg inches thick. The substratum is pink silt
loam to a depth of 60 inches.
lncluded with this soil in mapping are small areas of
Morval soils that have slopes of 12 to 25 percent. These
areas make up 10 to 18 percent of the map unit.
Permeability is moderate, and available water capacity
is high. Effective rooting depth is more than 60 inches.
Surface runoff is medium, and the erosion hazard is
severe.
This soil is used mainly for wildlife habitat, recreation,
some hay, and grazing.
The native vegetation on this soil is mainly need-
leandthread, wheatgrass, muttongrass, and sagebrush.
When the range is in poor condition, undesirable
weeds and annual plants are numerous. Properly manag-
rng grazing maintains and improves range condition. Re-
rlucing brush improves the range. Seedinq imnroves
- ,l'i:]. ii
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-*. -;i<--
'i"',,'.RlFLE AFEA, COLOBADO
and lho lowor f)itrt is [rrowtt lyritvt"'lly l;ln(ly lorrnr;tlrorrt lr
inches lhick. lltc sut.,:tlrithrr) ir, :;iurrl, c:olrlrlt::;, ;rrrrl
gravel to a depth of 60 rnches.
Permeability of tne Atencio sorl is rnoderate, an(t avail-
able water capacity is low. Effective rooting depth is 60
, inches or more. Surface runoff rs slow, and the erosion
hazard is slight.
The Azeltine soil is deep and well drained. Typically,
the suriace layer is reddish gray gravelly sandy loi.m
about I inches thick. The underlying layer is reddrsh
brown glavelly sandy loirm abcut 10 inches lhick. l'hc
substratum is calcareous sand, oravel, and cobbies to a
deplh of 60 inches or more.
Permeability of the Azeltine soil is rnoderately rapid,
and water capacity is very low. Effective rootinq depth is
about 60 inches or more. Surface runofl is slow, and the
erosion hazard is slight., These soils are used mainly for grazing and crops.
:. ,. .:.Alfalfa, small grains, potatoes, and grass-legume hay are' the main crops.
' '. This soil is irrigated mainly by lloodrng. Grassecl water-'", ways and minimum tillage prevent serious erosion. Covcr
-: Crops or stubble mulchrng in clrytarmed areas also
f reduce erosion.rri':: The native vegetation on these soils is mainly wheat-
grass, sagebrush, and ner-,dlc;rncilfrread.
: When range corrdition d<-'lt..rroratt.:s. IctrLrr; arrrl slrrrrlri
increase. When the ranqc is irr poor condilion, rrn(,()sirit-
ble weeds and annual plants Arc nuntorou5 Prttl;t-.rly
managrng grazing maintains ancl improves range condi-
tion. Seeding improves range in poor condition. Crested
wheatgrass, western wheatgrass, and Russian wildrye
are suitable for seeding. Preparing a seedbed and drillingi , the seed are good practices. Reducing brush improveiI the range.
, Pheasant, dove, rabbit, squirrel, and some deer fincj
lood and shelter on these soils, mainly in areas of crops.
Use of this soil for community developrnent or as a
source of construction material is [mited by the large
stones. Special design is needed for septic tank absorp-
tion fields because of seepage and the possibility of
polluting ground water.. This complex is in capability subclass lVs, irrigated,
and Vls, nonirrigated.
: g-Badland. This broadly def rned unit consists ofr r steep and very steep, neariy barren lancJ cJissected by
many intermittent drainage charrncl:i tlrat lravc cr.tt irrto
the soft shale and sandstorlc ol tlto Grecn Rrvor I-orrrrir-
tion and into the sofl shale and siltstorrc of tlre Wasatch,
,,"oMTncos, and Mesa Verde Forrnations. [Jadlancl occursr..;.:,lhrOuglrout the survcy arca, mainly orr stccpr footlrillr; artrJ
mOuntainsides lttal ltavc orrtcrol)s ol sllal(r r)r sirrrrlt;torrr.r.
About 85 percent or morc of tl're aroir is unvcgi)tali_'cl
The waler erosion hazarcJ is very scvcrc, ancJ crosion is
active.
Alrrltrl llr 1rr'rt.r'rtl rtl lltnl nliiir lrrrrl r:; ',trt:tll. r..ol.illrl
.ltt'lt'; ol I ,r,'t',rt, l.rtrrr,r, .iltj I ),,lltrr,j :,r)lll, I lr, ',,. '.t,,,:.
ll,tv(. ()trlv,r l,l':tr:..( l)l,illl r-:)\,,('r,1Jr,1,:rl1 :,catllr,'i't1 1t,rr'',:,
and jlrrrrpcr. I irr: v.rlue lor qrazrnq rs very lrmilcd Tlru,
trees provide a litlle protectroi.r and ccver lor lrvestock
and wildlrfe.
Badland is r-rnsuital.ric lor comntrrnit,., develcprlcni
,al{1land rs ln c.:-rpabrlit',, sirbClr,r:;r; \/lllc. nonirrCai{..(i,/\
( 1O-Qegay sandy loam. 1 to 6 percent slopes. Thrs
clectUlutt (iiir,rr,,'(j. rtCariv levrl tu oi:rrti,y' rolirrrtl so,l ts C;t
alluvial lans arrcJ srdes c{ valicvs. Ele',,Ltlion ranqcs irorn
5.00C to 6,500 feet Thrs sorl fornrec ir ailuvrunr dorrv,:d
lror,r rcci-Lrcd sandstcne anC snaic. The average arril,.;al
pre,cipitation i:r atrout 1,i rnches. thc averaq,J arrirLr;rl aii'
It.'rnl)eratrrr(: is atroul ,1 E tlciii'ees i:. .inii tlrp ;1y1,1 1.,,.
lrost-lrt:e p(rnod is airout 120 oavs.
Typically, tltr-- Surf ircc laycr is red or ycllc'"vr:rir rld
sancly loant atror,rt i4 inchr:s tltick. Tlrt: sLrbsorl i:; vt-:llorv-
islt retl Iirrcl santiy loirnr arbcrrt 10 incitr::; tltr(:k. I li,.r sulr-
stralutrt is yr,.llowish rcrj storry sarrriy loam to a d,.rililr oi
tiO inclres.
lnclrrdcd wrtlt this soil in nrappinq artl srnall Arc3lr ol
Olney and Ascalon soils that havc: sloper: of (i lr,r 12
percent. Thesc i:lrfras nritke up abotrl 5 to 10 Dcrcr-,rrt crf
lltc rnerl:l rrnil.
F)c,,rrrr,titlrtliiy i:i nrollr,r:rlr,ly r,ioit.t, irrtri;rv;trl.tlrlr,\..';tl,'r
capilcity t1i 191v, I-.ll('t:lrvi; rr.ri)lItr1 (j,'l)tl) rs; (iL) rri(.ir!,ri
.Stttlitcc rttnoll rs s;larw, irrtrl tltr) t,r(-,r;rrrrr lr;r;':trrl r.\ ln,\rl,:r.
el tc.
This soil rs used mainly for somt-. irr"rgated pasiL.rre arJ
hay and for grazing. Small acreages of wheat, barley,
and oats are grown.
Flooding and sorinklers are suitable fcr irrigating this
soil. Thrr: sorl is droughty and needs frequent irrigaticn lo
mature crops. Controlling the rate of water application
reduces piping and erosion.
l-he natrve veqetation on thrs sorl is mainly rvheal-
grass, necdlcanCthresd. and sagebrush.
Wlren range condition deteriorates, forbs and shrubs
increase. When the range is in poor conCition, undesii'a-
ble weeds and annual plants are numerous. Properly
managing grazing maintains anC improves range condr-
tion. Seeding improvcs range in poor condrticn. Cresied
whealgrass, westtrrn wheatgrass, and Fussian rvildrve
are surtable for seu-drng. Preparrng a scedbed and crrirrnq
the seed are goorl practices
COttOntail rallt:rl, sqtrirrt:1, nrarlirnirr!r Cjcrvu, Clrrrl'iir. itit-l
Sortt0 rrrrrlr: (,()(,r llnrl ltlrIrrt.tl Orr tltrs :;i)tl.
[.,lst: oI tirr:; sorl l(rr c,.)rrrr'nrtnitv dirvt,lc,!rilt'rrt anij il; ,i
SOLiICr:; Ol Ct]nstrrr(;trt)n trritlr:rrarl tS lrn)itr)d by :;,:cOiitti-,,
l;rrrlc stClnt:s, an(l cxc.rs;s frrtc'l;.-l-lliS s0il r; in (:itl)ill)rlrly :,Lrtri:l,ilrs.'1.: llie,, lrn(l;tlr'rj. irrll
lVc', tr0r n r r(.lill\r(j.
'l 1-t3egay sarrdy lonnr, 6 to 12 percent slopes.
Tlri:, ijr_.,,:p, wr--.!l Cjlarrrti.:(j. fIJ(J,,fijiitli,i..tr:.rrt)(l tr) rOllIr.] :.i. I
Jt*-' ' -;,"t e lgi
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IN Til;i Dlj;,i'liicT coilil.r Tlt ANI)l/A'inli Di vI5 iON lJ(). 5s'l^Tii ot,' coLott Do
cAsD No. w- l2l7
r-ll..tiD I.r'{ 1'r',\,'li.( C0URT IDrvrsion lio. 5 ,
DL-O 0 ,7197? Ii-rAt e oF COLORADO I.,..-.---:-. . .... {rt,,r.r; tt cLt.rt;: )nt I,Je 1.1 , I
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iN 'lill,l i.i/rrlDR Ot' TIID
Ai,j'i,I0AJ'i()N FOIi
V/,',?ilit nIGIiltS OF l(ATl'lRYM.
I'iILLIAIIS & TtiE COLOIUD0 Nr\T_
ICi'i:\L B/rlil( 0F DlitVER Co_exec*uto'is of Ehe EsEate of HenryP. l.lillia.ms, Jr.IN TI.IE COLORADO RIVER 'i
IN GARTIELD COUIITY
I. Name of Applicant
Address
5. ?he amount of water
7. The use of the water
,NULING Or THE RIIIENEB
, , AB,[o+U.TE .DFrnEB rOR :
UNDBN GROUND hIATER RIGIiTS
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, Glenwood Dprlngs, Colorado
And thc^Rcfercc- having made thc investi,ations requiredbv rirticlc 21 of chap-tcr r4B, cIR.s. r.i6rr-os-Ironaed doco herebymake the following ru1in6, to witt
This application was referred to the !/ater\/ater Divisj.on No. 5 on the legL day of Jrrf ,,
J' The teuL-description of the qtructure is: The well ls located insecEion 35, T.. 5 s., R. 90 w,. of tfre 6th p.M. at a polnt1550 feet SouEh of ihe worth ,ine and 800 feer tJest of theEast line of said Secrlon 35.
2. The name of tho structure is Dalry Bisement WeIl.
4. the dcpth of the well is 150 feet.
5' fhe date of initiation of appropriation is May \944.
Referee of
, L97L.Ikthryn E. I,Itlliams and The Colorado NationalBank of Denver
Rbute 2, Box 274
claimed is 0.t55 cublc foot per
- second of time.is domestic, commerci;l;'
that thio ruIin6; shnlI bc.colrlcuterkt oubjcct to Jurlicial revicw
8. The State Engineerrs nurnber is none.
9. ?he ltiority date is l,lay 31, tgto+,
LO. The date of the application was June 30, 1972.
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rt is thc ruling of the Rofcree tirat the statemonts in theapplication a.rc true and itot tto above dcscribod watcr right isa'pproved and grantcd thc indicatcri prioriiv;-ouuiu"t, however, to.all earlier priority ri56hts oi-otf,""u.
It ie accordingly ordcrcricf fcctivc upon filing wi tir" ttr"-Wotora.: providcd by Law.
*- o^, !iW?i;iy. sprin6s, colora,io this
ilr p:'ote:t v/aS f iled 1n thl i r.1i..io:.
Th r foregoing ru1 1nq 1s conf lrr::.i
ar' -rfli'ovcd, and is mfldo tho
Ju-;urcnt and Decrco of thls oourt,
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