HomeMy WebLinkAbout1.0 Applicationo o
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Application
for
AMENDED FINAL PLAT
Amending Tracts 29 and 36
and Portions of Tracts 28,30 a'nd37
Antlers Orchard Development PIat No. I
TRACTS OF LAND LYING IN SECTION 25
TowNSHIp 5 sourH RANGE 92 wEST oF THE 6* p.M.
GARFIELD COUNTY, COLORADO
Applicant:
Tom & Cecilia LaFrenz
2000 County Road 237
Silt, Colorado 81652
(970) 876-1900
Land Planning:Surveyor:
John L. Taufer & Associates, Inc.
Landscape Architectureiland Planning
P.O.Box227l
Glenwood Springs, Colorado 81602
(970) 94s-1337
Survco, Inc.
Professional Land Surveyors
1001 Grand Avenue Suite 205
Glenwood Springs, Colorado 81601
(e70) e28-8233
June 23, 2001
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Amended Plat Application Form
Applicant Name
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Subdivision Name:
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please attach a brief description of the amendments to take place, then sign and attach to this
application
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Location.Oa L4 Section ?6 TownshiP 6 Range n?'
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Change in Public
Existing Zoning:
Change in Easementt? @lto'
Lot(s) Size(s)
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Planning Department Review Fee:
County SurveYor Review Fee:
Total Filing Fee:
NO If Yes Where?
NO If Yes Where?u
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$100.00
$40.00
s140.00
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of tha cury of GAREIED
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MA.S J. IAEREM .n.t GE;IA A. IAEREITZ
and thc abov€d bargain€d prmisca
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xhosc tcaat addrc3r is 2000 County ROad 237, Silt, C0 81652
of tha Coury of GIREIE;D and stat. o{ Cotorado, of thr 3eo.rd tf,rt:ulTllESsETll, Th.t th! $id p.rty of th. f irst p.rt, for arid in cmid.ratim of th! s6 of dfi$290,000.00 I
Tto HUtoREo xtrETY lH(tlsAlto DoLLARS AXo 00/100TttS
ar1d othcr good atd vstt8bt. coroidcration to thc s.id party of th. firit p.rt in h..d prid by thr sid p.rtia of tie
36ond P!lt, thc raccipt {r.rcof ir hcreby cqrf"aacd ard acknoutcdecd, hr: grurtcd. bargairld, rotd ard corrcycd, md b7th6a Pc!3ats docs grilt, brrgein, satt, cwqT ard cmf im hto tia xid p.r!i.a of th. Goard par!, th.ir h.iB rard
assigns forevcr, mt in temncy in cmn but in joint t!!!'!gy.Jtt thc fottding d.lcribcd tot or Srrcel of trd.tying a.d bcing in thc CoLnry of GhREIE;D a.d Statc of Cotorldo, to rit:
SEE E(EIBIT iAi ATEACEIED EERETO }}ID I&DE A PART EEREF:
atso krcm as stre?t mtrbcr 2000 CiltrllY ROAD 237, SIII, O 81552
IOGETHEi rith att atd singuta. the herlditffits at appurtmoca tharcto bctorrging, or in ryrnrirc aFp.rtrining, r.ldthe rcwrsim a.td rlv.rsioc, rmirdcr and rffiirdcrs, rsts, i33G rd profits th.rofi rd att thr crtatc. right, tlttcintrr.3t, ctaim and daBnd dratsomr of thG s.id p.rt./ of tha fir.t p.rt, aith.r in tar ot cqJity,of, in and to th.
abova barglincd prai s6, rai th th. hcrcdi teunts ard aFp.JrtaarEaa.Io l{AvE AIO T0 [0O thc seid pcaiscs abovc b.rg.in.d and dcrcribcd, rith th. apFrtcnmc.., urto tha rid prrticr ofth. sccorid P.rt, th.ir hairs ard agignr forcvcr. lnd thc srid perty of thG fiBt Frt, fol hirctf, hir hriB, .lccuto.3,
and achini3tr.tors. doc cw.nst, grmt. hrgrin ard agre. to Erd Hith th. snid plrti6 of :ha s.cord part, thair hair3
and assigns, that at thc tim of thr rceal,irg and dcl,ivGry of ths prascnt3, hc ir rctt seizcd of tha priisc..bor.
cowcycd, as of good, sur!, pcrfcct, abeotut! ild indcfcrsibts c.t.ta of irhcritarrcc, in tu, in fcc sirpta, rrd hr goodright, fult Pol.rr a.d lerfut authotity to grant, b:rgain, sctt and cdlvly thr se in tEr.r.r ard form ar aforelid, rdthst tha su arc frcc ard ctcar fr6 atl fom ard other grantr, bargrin3, s.ls, tisl3, tu6, at...&trts andmcurbrarcg of rhatcvcr kird or mturc so+er;EIIGSE ET@.EL TN(E; AIID ASq'EqSiErrIS rcR TEE EAR 1995 }DID STIBSEtgOEITT EARS, IDID
luEqEql m 4 {ENrs, RESEllrAgtOlS, RESEr!:fgXOtrS, @vEtBArlS Il{D FjcES OF WI\y OFRE@RD, IF }I{Y;
..1d strta ot
in thc +rict and pcaeabl.c po:seim of s.id p.rtilr of thc 3cond frt, thc suryitr of
ard assigna of 3r.Eh survivor, agrimt att and avary Frscr or pfscrr trrfutty cttirir!thersf. thc seid party of thc fir:t p.rt shslt ard Hitt IJAiR XT ArD fOtEVEt DEFETO. fh.ptura(, thc ptural thG singutar, ..rd th. w. of zty gender rhrtl. bo rFpticrbt" to.u,
party of th. first p.rt h.. hcra,to sct his hlnd and scat th. dry ard ycrr first ebo,t
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SignGd, Sc.tcd ard octiv.fcd in thG Pr8mcr of
STATE Of COLOTAOO
Co6ty of
GEREIE.D
C
Mason & Morse Real Estate
801 Colorado Avenue
Glenwood Springs, C0 81601
sat)
SCAL)s.I
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Thr fo."going instrtmt r.r acknfltcdgcd brfora m thi3 d.y of lbtld€G 01, 1996
by .@I C. SlLr/mC[
r.y cmiition crpircr -y'1.1 A^aL 3t. t q n
Uitnara 6/ hard ard otfici.t srtt. '/
NMANY
PUBUC
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Fom l{rJ I UAIIAIIY oEEO . Io Joi^t Istrq'n2l:t85.221385 qE2t385
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BEGINNIIG AT A PONIT ON I'EE r8S? I.IITB Ol, SAID TRAC:I 30 I|XElel
nre cElrrER QUARTER CORIIBR Ot SArD SECTIOII 25 BBArui g 85
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BXCBPTITE TIIBRBFR,OIII :
A TRArr oP lallD IN lHE X1/2tlB1/{tfl1/{SB1/t OP SBclror 25'
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EN:NG IIIORB PARTIGJI.ARLT DESCR,IBBD AS FOLIOT9:
PIACE;
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CORNER OF
TIIEI{CE S
CORNER OF
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CORIiIER, OP
TI{ENCB N
BEGINNII|G
O DBCiREES 38'
SAID IR.ACT 35;
89 DEGRABS 38'
SAID E:RACT 35;
O DEGJR,EBS 55'
SAID TRACI 35;
O DBGRBBS 52'
36' B 328.93 FBEE tO Tr8 S@rElrsa
oo, r 585.32 ?BEr TO ttrl gGl'Elf8trr
17r r 329.05 FBEr rO AEE logrilssll
o7i r 33.00 FBEr TO IEB POI!tT OP
COUNIT OF GARFIEI.D
STATB OP COIPRADO
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JOHN L. TAUFEF| & ASSOCIATES, lNC.
Lendscape Anchitrectrune / Land Plenning
June 1 1, 2001
Garfield County Board of County Commisstoners
109 8th Street
Glenwood SPrings, Colorado 81601
Re: Final Amended Plat - LaFrenz Property
Dear Commissioners,
9O9 Colonado Avenue o Box ?271 o Glenrazood Spnings'CO El1604
(97o) 945-1337 o FAX (97A) 94=-7914
on behalf of Thomas & cecitia Lalrenz,I am pleased to submit this application to
request approval for a Final Amended Plat. The request consists of amending the lot
boundaries of five lSjpUttea Antler Orchard Development (AOD) Plat No'l.lots that are
owned by the LaFre:ii. The subject AOD lots were platted in 1906 and consist of Tracts
29 and36 and portions of Tracts 28,30 and37 respectively'
The property consists of 34.74acres and is situated in Section 25, Township 5 South'
il;.9) west of the La p.rra. The properry is situated adjacent to and south of the
LaFrerusubdivision Exemption that w;s recently approved by Garfield County'
The proposed amendment does not increase the number of lots previously platted'
The purpose of the proposed amendment is to provide a-better overall lot configuration
that is more suitable to the existing topography, thus offering more suitable building sites.
In addition, the proposed amendmint priviiei a more consistent sized lot compared to
the lot sizes that *.." pr.riously platted in 1906. In addition, the reconfiguration is
n"..rrury to avoid physical features that exist in some areas of the property'
Access
-l Au.t 3,i, 2..i +.1:i, 1('
Access to the amended lots will be from County Road237 ' Lots ffi8 andt' will have
access from an existing sixty foot (60') access easement that was originally platted with
the Antlers Orchard olvelopment ilatNo. 1 tracts' The alignment of this acc€ss
easement varies rfihtt from the existing easement that was originally platted' The
variation in alignment is necessary to avJid a livestock pond that exists on {,et-S. Iac'-cf 2*s
f*c.cr rY
Access to trat5 will be directly from county Road 237 and will occur on the northern
end of the lot. The owners wiil obtain the necessary access permits from the Garfield
County Road and Bridge DePartment'
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Potable Water
I have spoken with Dwight Whitehead, Division 5 Engineer, regarding exempt well
permits for the five (5) amended AOD lots. tn the opinion of Mr. Whitehead, this
represents a Catch 22 situation. He could issue the exempt well permits now, based on
the existing legal descriptions of each lot, but would rather wait until the Amended Plat is
approved so that each permit is issued based on the new legal description of each lot. His
issue is that he does not want to issue the permits now and have to come back and amend
the exempt well permits based on the amended lot configurations.
With regards to the physical supply of water, there are existing wells located within %
mile from the property that produce in excess of five (5) gallons of water per minute.
The LaFrenz well, located to the north of the AOD lots, produces eight (8) gallons per
minute.
Irrigation Water
Each lot owner will be entitled to Silt Project water that is currently owned by Tom &
Cecilia LaFrenz. A total of 40 acre feet of water will be allocated to the amended AOD
lots for outside irrigation use.
Sewage Disposal
The method of sewage disposal for all five (5) amended AOD lots will be by means of
ISDS. All of the lots are in excess of 5 acres in size which allows for adequate area to
accommodate ISDS systems.
Soils
The U.S.D.A. Soil Conservation Service soil survey mapping indicates that the AOD lots
are located within four (4) different soil types. The soil types include the following map
units: l)#21-Cushman-Lazearstonyloams;2)#34-Ildefonsostonyloam;3)#41-
Kim loam and 4) # 51 - Olney loam.
# 21 - Cushman-Lazear stony loams are found on the eastern end of the AOD lots.
Cushman =Lazear have severe limitations for site development, residential construction
and septic tank absorption fields.
# 34 - Ildefonso stony loams are found on the southeastern corner of the AOD lots.
These soils are similar to Cushman-Lazear soils in that the soil properties pose severe
limitations on site development.
2
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# 4l - Kim loams are located on the west end of the AOD lots. These soils have
moderate limitations for site development, residential construction and septic tank
absorption fields. These soils are well drained and are located on sloping terraces.
# 51 - Olney loams are located on the majority of the AOD lots. These soils are found on
nearly level alluvial fans and valley sides. These soils are similar to Kim loam soils
posing moderate limitations for site development, residential construction and septic tank
absorption fields.
All of the AOD lots include soil types with moderate limitations regarding site
development, buildirg-constructign and seu,age disposal systems. Although two (2) of
the lots, Lotsfi& g,Tr1r,A?r{rlrf"at#&ir-af ?ulh..,*-L-ear stony loams and Ildefonso. ,.. .stony loams sbils, site development is possible in these soils with appropriate mitigation
measures. We will include a Plat Note that requires lot owners to obtain engineered
fotrndations and septic systems if they elect to build in the Cushman-Lazear artd
Ildefonso soils.
Fire Protection
The AOD lots are located within the Burning Mountain Fire Protection Diskict boundary.
Don Zordel, District Chiel has indicated that the Fire Protection District will provide fire
protection services to the property.
Easements for Utilities, Access and Maintenance
The necessary easements for utilities, access and maintenance for the proposed amended
AOD lots are shown and described on the Amended Plat.
Compatibility With Surrounding Land Uses
The existing zoning of the property , A./R/RD, is compatible with the neighborhood
because the surrounding zoning is the same as the subject property and the proposed uses
are the same as the surrounding neighborhood. All of the proposed amended AOD lots
are consistent with the A/R/RD zoning regulations.
Conclusion
The owners request approval to reconfigure their five (5) existing Antler Orchard
Development Plat No.1 lots. They are not requesting an increase in the number of lots
but only an opporlunity to reconfigure their lots to make them more equal in size and to
provide a better relationship between lot and existing land.
The LaFrenz Amended Plat request has satisfied the requirements of the Garfield County
Zoning Resolution and the Garfield County Subdivision Regulations and is consistent
with the Garfield County Comprehensive Plan and the surrounding neighborhood.
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3
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I have attached three (3) copies of the Amended Final Plat for your review and comment.
We look forward to presenting this land use application to the Board of Cor-rnty
Commissioners at their earliest convenience.
If you have questions regarding this application or need additional information, please do
not hesitate to contact my office.
Sincerely
U-
John L. Taufer. Owners Representative
Attachments
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should be put up to keep livestock out, unwanted burn-
ing should be prevented, and the weflands should not be
drained. Natural wetland plants should be allowed to
grow. These soils also provide valuable summer range
for big game.
Seasonal flooding and depth to the water table limit
community development and recreation. Adequate drain-
age and protection from floods would be necessary
before development could be attempted. These soils can
be reserved as greenbelts or for other restricted uses.
These soils are in capability subclass Vlw, nonirrigat-
ed.
+ 21-Cushman-Lazear stony loams, 15 to 65 per-
cent slopes. These hilly to very steep soils are on
mountainsides and mesa breaks. Elevation ranges from
5,000 to 7,000 feet. The soils formed in sandstone and
shale residuum. The average annual precipitation is
about 13 inches, the average annual air temperatuie is
about 48 degrees F, and the average frost-free period is
about 125 days.
The Cushman soil makes up about 45 percent of the
map unit, and the Lazear soil makes up about 40 per-
cent. The Cushman soil is on the landscape where allu-
vium has accumulated to a greater depth over bedrock,
and the Lazear soil is on the more steep areas.
The Cushman soil is moderately deep and well
drained. Typically, the surface layer is grayish brown
stony loam about 3 inches thick. The subsoil is dark
grayish brown sandy loam about 8 inches thick. The
substratum is light brownish gray loam and very gravelly
loam. Shale and sandstone is at a depth of 32 inches.
Permeability ol the Cushman soil is moderate above
bedrock, and available water capacity is low. Eflective
rooting depth is 20 to 40 inches. Surface runoff is
medium, and the erosion hazard is severe.
The Lazear soil is shallow over bedrock and is well
drained. Typically, the surface layer is grayish brown
stony loam about 4 inches thick. The underlying material
is light brownish gray stony loam. Calcareous shale and
sandstone is at a depth of 16 inches.
Permeability of the Lazear soil is moderate above bed-
rock, and available water capacity is low. Effective root-
ing depth is 10 to 20 inches. Surface runotf is moderate-
ly rapid, and the erosion hazard is severe.
lncluded with these soils in mapping are small areas of
shale and sandstone outcrop and of lldefonso soils. The
lldefonso soils are deep and very stony and have large
acc'J;,lulalions of calcium carbonate. They are on very
steep, mesa breaks. These areas make up about 15
percent of the map unit.
These soils are used mainly for wildlife habitat and
grazing.
The native vegetation on these soils is mainly Utahjuniper and pinyon. The understory consists of Salina
wildrye, lndian ricegrass, beardless wheatgrass, galleta,
SOIL SURVEY
low phlox, stemless goldenweed, founruing saltbush, ser-
viceberry, shadscale, bitterbrush, and big sagebrush.
When the understory vegetation deteriorates, only a
few forbs and shrubs remain. Properly managing the
vegetation maintains wood production and grazing. Se-
lectively thinning the pinyon and junrper improves grazing
and provides firewood and posts. Steep slopes and the
erosion hazard affect harvesting.
These soils can produce about 6 cords of wood per
acre when trees more than 4.5 feet tall reach an aver-
age diameter of 5 inches.
Mule deer, gray squirrel, and cottontail rabbit find habi-
tat on these soils.
Use of these soils for community development and as
a source of construction materials is limited by depth to
bedrock and steep slopes.
This complex is in capability subclass Vlls, nonirrigat-
ed.
22-Dateman gravelly loam, 30 to 50 percent
slopes. This moderately deep, well drained, steep soil is
on mountainsides. Elevation ranges from 7,000 to 9,SOO
feet. This soil formed in sandstone and limestone residu-
um. The average annual precipitation is about 20 inches,
the average annual air temperature is about 38 degrees
F, and the average frost-free period is less than 75 days.
Typically, the upper part of the surface layer is very
dark grayish brown gravelly loam about 3 inches thick,
and the lower part is very dark grayish brown gravelly
sandy loam about 6 inches thick. The substratum is dark
yellowish brown very gravelly sandy loam. Limestone or
sandstone bedrock is at a depth of 34 inches.
Included with this soil in mapping are small areas of
Farlow, Cochetopa, and Lamphier soils on the steeper
parts of the landscape. They make up about 5 to 15
percent of the map unit.
Permeability is moderate, and available water capacity
is low. Effective rooting depth is 20 to 40 inches. Surface
runoff is medium, and the erosion hazard is moderate.
This soil is used mainly for wildlife habitat and grazing.
The native vegetation on this soil is mainly Gambel
oak, serviceberry, and mountain brome. A few small
areas have some Douglas-fir.
When range condition deteriorates, forbs and shrubs
increase. When the range is in poor condition, Kentucky
bluegrass, undesirable weeds, and annual plants are nu-
merous. Properly managing grazing maintains and im-
proves range condition. Seeding and controlling brush
are generally unsuitable because of the steep slopes.
Elk, mule deer, blue grouse, snowshoe rabbit, and
squirrel find habitat on this soil.
Use of this soil for community development and as a
source of construction material is limited by steep slopes
and depth to rock.
This soil is in capability subclass VIle, nonirrigated.
BIFLE AREA, COLORADO o o
ranges from 5,000 to 6,500 feet. This soil formed in
mixed alluvium derived primarily from basalt. This soil
has a thin intermittent cap of reddish eolian material. The
average annual precipitation is about 14 inches, the
average annual air temperature is 46 degrees F, and the
average frost-free period is about 125 days.
Typically, the surface layer is brown stony loam about
8 inches thick. The underlying material is white, very
strongly calcareous very stony loam to a depth of 60
inches.
lncluded with this soil in mapping are small areas of
Potts and Ascalon soils on less sloping positions. These
areas make up 5 to 15 percent of the map unit.
Permeability is moderately rapid, and available water
capacity is low. Effective rooting depth is more than 60
inches. Surface runotf is medium, and the erosion hazard
is moderate.
This soil is used mainly for grazing and wildlife habitat.
The native vegelation on this soil is mainly pinyon and
Utah juniper. The understory consists mostly of lndian
ricegrass, wheatgrass, junegrass, serviceberry, bitter-
brush, and big sagebrush.
When the understory vegetation deteriorates, grasses
almost disappear and forbs and shrubs increase. Proper-
ly managing the vegetation maintains wood production
and grazing. Selectively thinning the pinyon and juniper
improves understory grazing and provides firewood,
posts, and Christmas trees.
This soil is suited to production of pinyon and Utahjuniper. lt can produce 9 cords of wood per acre when
trees more than 4.5 feet tall reach an average diameter
(at one foot) of 5 inches. The low available water capac-
ity affects survival of tree seedlings.
Mule deer, chukar, wild turkey, gray squirrel, and cot-
tontail rabbit find habitat on this soil.
Community development is limited by large stones and
steep slopes. Structures to divert runoff aie needed for
roads.
This soil is in capability subclass Vls, nonirrigated.
X Sl-ltOefonso stony Ioam, 25 to 45 percent stopes.This deep, well drained, hilly to steep boil is on mesa
breaks, sides of valleys, and alluvial fans. A small portionof this unit is on very steep to extremely steep mesaescarpments. Elevation ranges from 5,000 to 6,500 feet.This soil formed in mixed ajiuvium derived primarily frombasalt. This soit has a thin intermittent cip of r6OOisneolian material. The average annual precipitation is about14 inches, the average ainual air temperature is about
J!_degrees F, and the average frost-free period is about125 days.
^ Typically, the surface layer is brown stony loam aboutu tnches thick. The underlying material is white, very
Itgngty calcareous very st6n/ toam to a depth of 60nches.
^
lncluded with this soil in mapping are small areas ofrotts and Ascalon soils on less steep and depressional
23
positions. These areas make up about 5 to 15 percent of
the map unit.
Permeability is moderately rapid, and available water
capacity is low. Etfective rooting depth is more than 60
inches. Surface runoff is medium, and the erosion hazard
is severe.
lldefonso soil is used mainly tor grazing and wildlife
habitat.
The native vegetation on this soil is mainly pinyon and
Utah juniper. The understory consists of lndian ricegrass,
wheatgrass, junegrass, serviceberry, bitterbrush, and big
sagebrush.
When the understory vegetation deteriorates, grasses
almost disappear and forbs and shrubs increase. Proper-
ly managing the vegetation maintains wood production
and ground cover. The value for grazing is low becauseof steep slopes and tree cover. Firewood, posts, and
Christmas trees can be harvested on the more gently
sloping areas.
This soil is suited to production of pinyon and Utah
juniper. lt can produce 9 cords of wood per acre when
trees more than 4.5 feet tall reach an average diameter
(at one foot) of 5 inches. The low available water capac-
ity affects survival of tree seedlings. Steep slopes and
severe erosion hazard affect harvesting.
Mule deer, chukar, wild turkey, gray squirrel, and cot-
tontail rabbit find habitat on this soil.
Community development is limited by large stones and
steep slopes. Structures to divert runoff are needed for
roads.
This soil is in capability subclass Vlle, nonirrigated.
35-lldefonso-Lazear complex, 6 to 65 percent
slopes. Moderately sloping to very steep soils are on
hillsides and mesa breaks. Elevation ranges from 5,000
to 6,500 feet. The lldefonso soil formed in very calcare-
ous, mixed, stony alluvium derived mainly from basalt,
and the Lazear soil formed in shale and sandstone re-
siduum. 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
125 days.
The lldefonso soil makes up about 50 percent of the
unit, the Lazear soil makes up about 30 percent, and
soils of minor extent make up 20 percent.
The lldefonso soil is deep and weil drained. Typically,
the surface layer is brown stony loam about 8 inches
thick. The underlying material is white, very strongly cal-
careous very stony loam to a depth of 60 inches.
Permeability of the lldefonso soil is moderately rapid,
and available water capacity is low. Etfective rooting
depth is more than 60 inches. Surface runoff is medium,
and the erosion hazard is moderate.
The Lazear soil is shallow over shale bedrock and is
well drained. Typically, the surface layer is grayish brown
gravelly loam about 4 inches thick. The underlying mate-
26 o o SOIL SURVEY
Surface runoff is slow, and the erosion hazard is moder_
ate.
This soil is used mainly for crops, hay, and pasture.
Alfalfa, small grains, and grass or grass-l6gume mixtures
are grown.
This soil is irrigated by flooding or furrows. Sprinklers
are also suitable. Drop structures in ditches control water
and prevent excessive ditch erosion.
The native vegetation on this soil is mainly wheat_
grasses, needleandthread, 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. Crested wheatgrass,
western wheatgrass, and Russian wildrye are suitadle for
seeding. Preparing a seedbed and drilling the seed aregood practices.
Cottontail rabbit, ground squirrel, and pheasant find
habitat on this soil.
Use of this soil for community development and as asource of construction material is limited by low strength.
.. .This soil is in capability subclasses llle, irrigated, indlVc, nonirrigated.
# 1l:\r^.toam, 6 to 12 percent stopes. This deep,well drained, moderately sloping to rolling soil is on allu_vial fans and benches. Elevation ranges from 5,000 toS,000 feet. This soil formed in alluvium derived from
shale and sandstone. The average annual precipitation isabout 12 inches, the average ahnual air tempbrature is
about 48_degrees F, and the average frost-free period isabout 125 days.
Typically, the surface layer is yellowish brown or lightyellowish brown loam about 17 inches thick. The undir-lying material is light brownish gray loam to a depth of60 inches. ln places the underlying material is stratifiedwith fine sandy loam.
lncluded with this soil in mapping are small areas ofArvada and Potts soils that have- slopes of 6 to .12
percent. These areas make up 5 to 15 percent of themap unit.
. ??rT"q9ility is moderate, and available water capacityis high. Effective rooting depth is 60 inches or hore.
Surface runoff is slow, and the erosion hazard is moder_
ate.
This soil is used mainly for crops, hay, and pasture.
Alfalfa, small grains, and grass or grass-legume mixtures
are grown.
This soil is irrigated by flooding and furrows. Sprinklersare also suitable. Drop structures in irrigation ditchescontrol water and prevent excessive ditch erosion. Keep_ing the soil in hay or pasture at least three-fourths of thetime helps to control erosion.
The native vegetation on this soil is mainly wheat-grass, needleandthread, 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. Crested wheatgrass,
western wheatgrass, and Russian wildrye are suitable for
seeding. Preparing a seedbed and drilling the seed are
good practices.
Cottontail rabbit, ground squirrel, and pheasant find
habitat on this soil.
Use of this soil for community development and as a
source of construction material is limited by low strength
and steep slopes.
This soil is in capability subclasses lVe, irrigated, and
Vle, nonirrigated.
42-Lamphier loam, 15 to 50 percent slopes. This
deep, well drained, steep soil is on fans and mountain-
sides. Elevation ranges from 7,500 to j 0,000 feet. This
soil formed in residuum from sandstone and shale. The
average annual precipitation is about 21 inches, the
average annual air temperature is about 40 degrees F,
and the frost-free period is less than 75 days.
Typically, the surface layer is dark brown loam about
30 inches thick. The underlying material is reddish brown
and dark reddish brown loam to a depth of 60 inches.
lncluded with this soil in mapping are small areas ofAlmy soils and Rock outcrop. The Almy soils are at
lower elevations. These areas make up 5 to 1O percent
of the map unit.
. Permeability is moderate, and available water capacityis high. Effective rooting depth is 60 inches or more.
Surface runoff is slow, and the erosion hazard is slight.
This soil is used mainly for grazing, wildlife habitat, ind
recreation.
The native vegetation is aspen and an understory of
bromes, elk sedge, wildrye, wheatgrass, peavine, coium-
bine, snowberry, serviceberry, and chokecherry.
When the understory vegetation deteriorates, forbs,
shrubs, and Kentucky bluegrass increase. properly man-aging grazing maintains and improves the understory
vegetation.
This soil is suited to production of quaking aspen. lt
can produce 4,050 cubic feet of wood per acre or 6,g00board feet of timber from a fully stocked, even-aged
stand of 8O-year-old trees. At the present there is no
commercial harvest of the aspen. Steep slopes affect
harvesting, and special attention is needed to reduce soil
loss during harvest.
Mule deer, elk, blue grouse, and snowshoe rabbit find
habitat on this soil.
Septic tank filter fields, community development, androads are limited by steep slopes. Surface runoff from
snowmelt increases the erosion hazard on cuts and fills.Seeding reduces the erosion hazard. Roads can be de-
30
degrees F, and the average frost-free period is about
125 days.
Typically, the surface layer is grayish brown loam
about 12 inches thick. The subsoil is grayish brown and
light gray sandy clay loam about 21 inches thick. The
substratum is light gray gravelly sandy clay loam or very
gravelly sandy loam to a depth of 60 inches.
lncluded with this soil in mapping are small areas of
Heldt, Potts, and Kim soils that have slopes of 3 to 6
percent. These areas make up 5 to 15 percent of the
map unit.
Permeability is moderate, and available water capacity
is moderate. Effective rooting depth is 60 inches or
more. Surface runoff is slow, and the erosion hazard is
moderate.
This soil is used mainly for irrigated crops and hay.
Alfalfa, small grains, corn for silage, and grass or grass-
legume mixtures are grown. Small acreages are in fruits,
including apples, peaches, and apricots. lsolated areas
are used for grazing.
This soil is irrigated by furrows and flooding. Sprinklers
are also suitable. Drop structures in irrigation ditches
help to control water and prevent excessive ditch ero-
sion.
The native vegetation on this soil is mainly wheat-
grass, needleandthread, 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 deteriorated range. Seed-
ing improves range in poor condition. Crested wheat-
grass, western wheatgrass, and Russian wildrye are suit-
able for seeding. Preparing a seedbed and drilling the
seed are good practices.
Cottontail rabbit, squirrel, pheasant, and some mule
deer find habitat on this soil.
Community development and recreation are limited by
low strength.
This soil is in capability subclasses llle, irrigated, and
lVe, nonirrigated.
)F Sr-Olney !oam, 6 to 12 percent slopes. This deep,
well drained, moderately sloping to rolling soil is on allu-
vial fans and sides of valleys. Elevation ranges from
5,000 to 6,500 feet. This soil formed in alluvium derived
from sandstone and shale. The average annual precipita-
tion is about 14 inches, the average annual air tempera-
ture is about 48 degrees F, and the frost-free period is
about 125 days.
Typically, the surface layer is grayish brown loam
about 12 inches thick. The subsoil is grayish brown and
light gray sandy clay loam about 21 inches thick. The
substratum is light gray gravelly sandy clay loam and
very gravelly sandy loam to a depth of 60 inches.
lncluded with this soil in mapping are small areas of
Heldt, Potts, and Kim soils that have slopes of 6 to 12
SOIL SURVEY
percent. These areas make up 5 to 15 percent of the
map unit.
Permeability is moderate, and available water capacity
is moderate. Effective rooting depth is 60 inches or
more. Surface runoff is medium, and the erosion hazard
is moderate.
This soil is used mainly for irrigated hay, fruits, and
grazing. Grass-legume mixtures and apples, peaches,
and apricots are grown.
This soil is irrigated by furrows and flooding. Sprinklers
are also suitable. Drop structures in irrigation ditches
help to control water and prevent excessive ditch ero-
sion. Keeping a grass or legume cover on this soil at
least three-fourths of the time controls erosion.
The native vegetation on this soil is mainly wheat-
grass, needleandthread, 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. Crested wheatgrass,
western wheatgrass, and Russian wildrye are suitable for
seeding. Preparing a seedbed and drilling the seed are
good practices.
Cottontail rabbit, squirrel, pheasant, and some mule
deer find habitat on this soil.
Community development and recreation are limited by
steep slopes and low strength.
This soil is in capability subclass lVe, irrigated and
nonirrigated.
S2-Parachute loam, 25 to 65 percent slopes. This
moderately deep, well drained, hilly to very steep soil is
on north- and east-facing mountainsides. Elevation
ranges from 7,500 to 8,700 feet. This soil formed in
residuum from sandstone. The average annual precipita-
tion is 20 inches, the average annual air temperature is
about 40 degrees F, and the average frost-free period is
less than 75 days.
Typically, the surface layer is grayish brown loam
about 5 inches thick. The upper part of the subsoil is
very dark grayish brown and brown loam about 13
inches thick, and the lower part is light yellowish brown
extremely channery loam about 11 inches thick. Hard,
fractured sandstone bedrock is at a depth of 29 inches.
lncluded with this soil in mapping are small areas of
Rhone and lrigul soils. The Rhone soils are in concave
positions. These areas make up 10 to 15 percent of the
map unit. lrigul soils are on ridge crests.
Permeability is moderate, and available water capacity
is low. Effective rooting depth is 20 to 40 inches. Surface
runoff is medium, and the erosion hazard is moderate.
This soil is used mainly for wildlife habitat and limited
grazing.
a
Adjacent Property Owners
Within 200'
Ruth J. Kary
407 County Road 250
Silt, Colorado
81652
Donald W. Larson
335 County Road 250 #A
Silt, Colorado
81652
Perry & Angela Lynn Urban
411 County Road 250
Silt, Colorado
816s2
John E. & Lisa C. Moore
1 887 County Road 237
Silt, Colorado
8t652
John R. & Peggy Spangler
1823 CountyRoad23T
Silt, Colorado
81652
Richard J. Murr
37659 Highway 6
New Castle, Colorado
81647
Arloa & Neil R. Myers
326 331/2 Road
Palisade, Colorado
8t526
Farmer's Irrigation Company
Attn: Elsa Pyles
P.O. Box 8
Silt, Colorado 81652
A&EDiemozLLLP
214 Pine Street
Glenwood Springs, Colorado
8160 r
Michael D. & Colista J. Larsen
2165 CountyRoad23T
Silt, Colorado
8t652
Daniel J. Dimaria
P.O. Box 6724
Snowmass Village, Colorado
81615
Bureau Of Land Management
P.O. Box 1009
Glenwood Springs, Colorado
81602
Lyman E. & Donna K. Fogel
501 Ingersoll Lane
Silt, Colorado
81652
ZangFamily Trust
415 County Road 250
Silt, Colorado
816s2
Michael Weinstein;
Elizabeth Green
185 Orchard Lane
Glenwood Springs, Colorado 81601
Mineral Rights Owners
Arlis M. Brooks
P.O. Box 241
Escalante, Utah 84726
Corrine P. Stahl
Attn: June Roofener
21 Oak Hill Road
GreenBriar, Arkansas 72058
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(D
BUILDING & PLAN N I N G D E PART\VT E NT
August 14,2OOl
Tom & Cecilia LaEreru
2000 County Road237
silt, co 91652
RE:Antlers Orchard I)evelopment plat No. I Amended plat
Dear Tom & Cecilia:
Your request for an Amended Final Plat, as identified on the encrosed public notice form, has been scheduredforapublicmeetingbeforeth"G;;i;ct*tyil*d;rEo*rrcommissionersattheirseptember
ro,20or,E#'"hffi ilEffi #1":;Tffi?:"{;Shr*,n*m,,:,;,xy::rynoodiui,egor,
your representative be present at the time of the -"",irf '''rED' \-\r o r ou I ' lt ls suggested that you and or
A copy of the enclosed public notice and all attachments must be mailed, by certified ma,, retum-receiptrequested' to all immediately adjoining property omers and property "*r.^ *i,hin 200 ft. of the proposedamended plat' It is also nt"tt'uty to t"ia th. .u." ,oti*il -inerar ;*il;J lessees ofmineral Jwners ofrecord' by retum-receipt mail' All notices shall be mailea at reast fifteen rrrl},o not more than thirty (30)days prior to the meeting' The site must be posted *i;;; enclosed rotir" i, u rocation that is clearry andconspicuously visible form a public right-of- way, atr"*i iiauys and not -or" ,rr* 30 days in advance ofthemeeting' The applicant shall be ."rp.iribl" f";;;]';"g ,rr"" ,oti"r. _Tg ,h;iGsent proof of ma,ing at orprior to the meeting' Please verify,ii" *r*u"y of ail eiclosures and if you discover any erors, contact thisoffice immediately.
Ifyou have further questions or concerns regarding the meeting orpubric notice requirements, prease contactthis office.
Sincerelv.
C^ffi
Cathi Edinger
Planning Technician
Enclosure
Gaffield Coun U
Cc: John Taufer
109
'th
Street, Suite 303, Glenwood Springs, Colorado gl60l(970) 945-8212 e7q 255_7972 ' Fo*, (g70) 384_3470
ryd&{.-t .th4a; t/'{ll
Qarfield Counfy Planning Department Todoy's r"P (t C
F gocc O Plonning Commission tr BOA
Project Nome: AfllWS QRe hrr4.l loorn(n+ Cp, ?h+ + I
Type of APPlicotion:
tr Special Use Permit
O Conditionol Use Permit
O SubdivisionExemPtion
B Subdivision Finol Plot
,.(suUdivision Finol Plot Amendment
D Subdivision Preliminory Plon
tr Amendment to
tl other
To do
ffRuulic Heoring
$euUtic Meeting
tr Consent Agendo
Est. Durotion:
Est. Durotion:
ol\.
c^A m c-on6iB*€,flt ,"i.H^t-i*F 4r7r.S ln 'fl"€n{.e,a-
Dote
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Site Locotion:
o 1
1
Section / TownshiP / Ronge:
Time:
f 1:15 pmtr 1o:oo om
^1,
R
5 K? a i^l
on
-To nut q- Cb.i /,'o L"o€g=r\-z--Applicont:
Reguested Action:F Approvol O Deniol
Item Advertised? tr Yes ff Yes, when?
Stoff Plonner:
Mork Beon
Kit Lyon
Rondy Russell
Greg Butler
A No
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BhEE?H' ao. (,1) *,,,^k L--,"^*u
622L
2271 PH.94s-'t337
GLENWOOD SPRINGS, CO 81602 82-26{,/1021 2tp /L.6/ai
Bank ol Colorado
ot*
DATE
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L TAUFER AND ASSOCIATES, INC.
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