HomeMy WebLinkAbout20051947.tiff EEC
July 30, 2002
EARTH ENGINEERING
Mn Bob Parsons CONSULTANTS, INC.
40455 Skylark Drive
Fort Collins, Colorado 80524
Re: Geologic Evaluation
Peace Haven Estates
Weld County, Colorado
EEC Project No. 1022125
Mr. Parsons:
Earth Engineering Consultants, Inc. (EEC)personnel have completed the geologic evaluation you
requested for the referenced project. That evaluation was completed by reviewing readily available
data concerning soil and groundwater conditions at the site, principally through review of United
States Geologic Society(USGS)/Colorado Geologic Society(CGS) and Department of Agriculture
Soil Conservation Service (SCS)published information. A listing of the references reviewed as a
part of the geologic hazard study is included with this report. We understand the lots at the
referenced project will be at least 5 acres in size, therefore no percolation testing was completed as
a part of this evaluation.
The Peace Haven Estates project is located in Section 10, T7N, R67W of the 6(h P.M. in Weld
County, Colorado. The development parcel includes approximately 48.5 acres. Site drainage is to
the southeast with total elevation change across the site on the order of 30 feet.A diagram indicating
the approximate location of the development is included with this report.
The attached soil classification map includes demarcation of those soil groupings identified on the
site by SCS soil maps. SCS descriptions of those soil types are provided with this report. In general,
the near surface soils at this site appear to be a blend of low plasticity clay loam and fine sandy loam
soils. The SCS information indicates the property would be expected to have groundwater at depths
of 5 to 20 feet.
According to the geologic maps of the area, the surficial materials mapped consist of eolean(wind
deposited) soils from the Upper Holocene and Pleistocene geologic period. The eolean materials
overlie the Upper Transition Member of the Pierre Shale bedrock formation. The Upper Transition
Member consists of sandstone with sandy shale layers. According to SCS data, depth to bedrock in
CENTRE FOR ADVANCED TECHNOLOGY
2301 RESEARCH BOULEVARD, SUITE 104
FORT COLLINS, COLORADO 80526
(970) 224-1522 (FAx) 224-4564 2005-1947
Earth Engineering Consultants,Inc.
EEC Project No. 1022125
July 30, 2002
Page 2
the Olney series is greater than 60 inches; however, bedrock in the Renohill series could be
encountered between 20 and 40 inches below present site grades.
Based on our review of the site as outlined above, we expect the near surface soils could be used for
support of lightly loaded residential structures. The near surface soils appear to exhibit a low
potential for volume change with variation in moisture content; however, the Renohill series may
exhibit moderate to high swell potential. SCS information indicates the Olney series would be
expected to exhibit acceptable percolation rates for on-site septic systems; however, the Renohill
series may exhibit slow percolation rates or shallow bedrock.
During our review of available site data, we did not identify potential geologic hazards as outlined
in H.B. 1041. Shallow bedrock and slower percolation rates would be expected in the area of the
Renohill Series. In addition, we did not identify economically recoverable mineral resources as
defined in H.B. 1041 at this site.
The evaluation for this report was based on a review of readily available public information for the
property. Specific site data should be developed for individual residences and septic fields once the
locations of those improvements are identified.
We appreciate the opportunity to be of service to you on this project. If you have any questions
concerning the enclosed information or require additional information, please do not hesitate to
contact us.
Very truly yours,
Ear ,.r.'.sT•.eering Consultants, Inc.
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Mic' :'' : 'oley, P.E.
Project Engineer
WELD COUNTY ROAD 84
SUBJECT
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47
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NOT TO SCALE
SCS SOIL SERIES MAP
PEACE HAVEN ESTATES - WELD COUNTY, COLORADO
PROJECT NO: 1022125 DATE: JULY 2002
47—Olney fine sandy loam, 1 to 3 percent slopes.
This is a deep, well drained soil on plains at elevations of ble years to 1,800 pounds in unfavorable years. As range
4,600 to 5,200 feet. It formed in mixed outwash deposits. condition deteriorates, the sand bluestem, sand reedgrass,
Included in mapping are small areas of soils that have a and switchgrass decrease and blue grams, sand dropseed,
dark surface layer. Some small leveled areas are also in- and sand sage increase. Annual weeds and grasses invade
eluded the site as range condition becomes poorer.
Typically the surface layer of this Olney soil is grayish Management of vegetation on this soil should be based
brown fine sandy loam about 10 inches thick. The subsoil on taking half and leaving half of the total annual produc-
is yellowish brown and very pale brown sandy clay loam tion. Seeding is desirable if the range is in poor condition.
about 14 inches thick. The substratum to a depth of 60 Sand bluestem, sand reedgrass, switchgrass, sideoats
inches is very pale brown,calcareous fine sandy loam. grams, blue grams, and pubescent wheatgrass are suite-
Permeability and available water capacity are ble for seeding. The grass selected should meet the
moderate. The effective rooting depth is 60 inches or seasonal requirements of livestock. It can be seeded into
more. Surface runoff is medium, and the erosion hazard is a clean, firm sorghum stubble, or it can be drilled into a
low. firm prepared seedbed. Seeding early in spring has
In litigated areas this soil is suited to all crops corn- proven most successful.
monly grown in the area, including corn, sugar beets, Windbreaks and environmental plantings are generally
beans, alfalfa, small grain, potatoes, and onions. An exam- suited to this soil. Soil blowing, the principal hazard in
ple of a suitable copping system is 3 to 4 years of alfalfa establishing trees and shrubs, can be controlled by cul-
followed by corn, corn for silage, sugar beets, small grain, tivating only in the tree row and by leaving a strip of
or beans. Land leveling, ditch lining, and installing vegetation between the rows. Supplemental irrigation
pipelines may be needed for proper water application. All may be needed at the time of planting and during dry
methods of irrigation are suitable, but furrow irrigation is periods.Trees that are best suited and have good survival
the most common. Barnyard manure and commercial fer- are Rocky Mountain juniper, eastern redcedar, ponderosa
Wien-are needed for top yields. pine, Siberian elm, Russian-olive, and hackberry. The
In nonirrigated areas this soil is suited to winter wheat, shrubs best suited are skunkbush sumac, lilac, and Siberi-
barley, and sorghum. Most of the acreage is planted to an peashrub.
winter wheat. The predicted average yield is 28 bushels Wildlife is an important secondary use of this soil. The
per acre. The soil is summer followed in alternate years cropland areas provide favorable habitat for ring-necked
to allow moisture accumulation. Generally precipitation is pheasant and mourning dove. Many nongame species can
too low for beneficial use of fertilizer. be attracted by establishing areas for nesting and escape
Stubble mulch farming, striperopping, and minimum dl- cover. For pheasants, undisturbed nesting cover is essen-
lage are needed to control soil blowing and water erosion. tial and should be included in plans for habitat develop-
Terracing also may be needed to control water erosion. went, especially in areas of intensive agriculture. Range-
The potential native vegetation on this range site is land wildlife, for example, the pronghorn antelope, can be
dominated by sand bluestem, sand reedgrass, and blue attracted by developing livestock watering facilities,
grams Needleandthread, switchgrass, sideoats grama, managing livestock grazing, and reseeding where needed
and western wheatgrass are also prominent. Potential Rapid expansion of Greeley and the surrounding area
production ranges from 2,200 pounds per acre in favora- has resulted in urbanization of much of the Olney soil 4
This soil has good potential for urban and recreational
development. The only limiting feature is the moderately
rapid permeability in the substratum, which causes a
hazard of ground water contamination from sewage
lagoons. Lawns, shrubs, and trees grow well. Capability
subrlac5 IIe irrigated, We nonirrigated; Sandy Plains
range site.
USDA SOIL CONSERVATION SERVICE
SOIL GROUP DESCRIPTION
OLNEY SERIES
Forth Fnainpprinn rnncnitnntc
48—Olney fine sandy loam, 3 to 5 percent slopes.
This is a deep, well drained soil on plains at elevations of
4,600 to 5,200 feet. It formed in mixed outwash deposits. Windbreaks and environmental plantings are generally
Included in mapping are small areas of soils that have a suited to this soiL Soil blowing, the principal hazard in
dark surface layer and small areas of soils that have establishing trees and shrubs, can be controlled by cul-
sandstone and shale within a depth of 60 inches. tivating only in the tree row and by leaving a strip of
Typically the surface layer of this Olney soil is grayish vegetation between the rows. Supplemental irrigation
brown fine sandy clay loam about 8 inches thick. The sub- may be needed at the time of planting and during dry
soil is yellowish brown and very pale brown fine sandy periods. Trees that are best suited and have good survival
loam about 12 inches thick The substratum to a depth of are Rocky Mountain juniper, eastern redcedar, ponderosa
60 inches is very pale brown, calcareous fine sandy loam. pine, Siberian elm, Russian-olive, and hackberry. The
Permeability and available water capacity are shrubs best suited are skunkbush sumac, War and Siberi-
moderate. The effective rooting depth is 60 inches or an peashrub.
more. Surface runoff is medium, and the erosion hazard is Wildlife is an important secondary use of this soil The
low. cropland areas provide favorable habitat for ring-necked
In irrigated areas this soil is suited to the crops corn- pheasant and mourning dove. Many nongame species can
monly grown in the area. Perennial grasses and alfalfa or be attracted by establishing areas for nesting and escape
close grown crops should be grown at least 50 percent of cover. For pheasants, undisturbed nesting cover is essen-
the time. Contour ditches and corrugations can be used in tial and should be included in plans for habitat develop-
irrigating close grown crops and pasture. Furrows, con- went, especially in areas of intensive agriculture. Range-
tour furrows, and cross slope furrows are suitable for row land wildlife, for example, the pronghorn antelope, can be
crops. Sprinkler irrigation is also desirable. Keeping til- attracted by developing livestock watering facilities,
lege to a minimum and utilizing,crop residue help to con- managing livestock grazing, and reseeding where needed.
trol erosion. Maintaining fertility is important. Crops Rapid expansion of Greeley and the surrounding area
respond to applications of phosphorus and nitrogen. has resulted in urbanization of much of this Olney soil.
In nonirrigated areas this soil is suited to winter wheat, The soil has good potential for urban and recreational
barley, and sorghum. Most of the acreage is planted to development The only limiting feature is the moderately
winter wheat. The predicted average yield is 25 bushels rapid permeability in the substratum, which causes a
per acre. The soil is summer fallowed in alternate years hazard of ground water contamination from sewage
to allow moisture accumulation. Generally precipitation is lagoons. Lawns, shrubs, and trees grow well. Capability
too low for beneficial use of fertilizer. subclass IIIe irrigated, IVe nonirrigated; Sandy Plains
Stubble mulch fanning, striperopping, and minimum til- range site.
lage are needed to control soil blowing and water erosion.
Terracing also may be needed to control water erosion.
The potential native vegetation on this range site is
dominated by sand bluestem, sand reedgrass„and blue
grams. Needleandthread, switchgrass, sideoats grams,
and western wheatgrass are also prominent Potential
production ranges from 2,200 pounds per acre in favora-
ble years to 1,800 pounds in unfavorable years. As condi-
tion deteriorates, sand bluestem, sand reedgrass, and
switchgrass decrease and blue grams, sand dropseed, and
sand sage increase. Annual weeds and grasses invade the
site as range condition becomes poorer.
Management of vegetation on this soil should be based
on taking half and leaving half of the total annual produc-
tion. Seeding is desirable if the range is in poor condition.
Sand bluestem, sand reedgrass, switchgrass, sideoats
grams, blue grams, pubescent wheatgrass, and crested
wheatgrass are suitable for seeding. The grass selected
should meet the seasonal requirements of livestock. It can
be seeded into a clean, firm sorghum stubble, or it can be
drilled into a firm prepared seedbed. Seeding early in
spring has proven most successfuL
USDA SOIL CONSERVATION SERVICE
SOIL GROUP DESCRIPTION
OLNEY SERIES
Earth Engineering Consultants
57—Renohill clay loam, 3 to 9 percent slopes. This is
a moderately deep, well drained soil on upland hills and Closely spaced contour ditches can be used in irrigating
ridges at elevations of 4,850 to 5,200 feet it formed in close grown crops. Contour furrows should be used for
residuum from shale. Included in mapping are small areas row crops. Applications of barnyard manure and commer- .
of soils that have shale deeper than 40 inches. vial fertilizer help to maintain good production. Keeping
Typically the surface layer is grayish brown clay loam tillage to a minimum and utilizing crop residue are impor-
about 9 inches thick. The subsoil is grayish brown and tant.
pale brown clay loam about 12 inches thick. The sub- The potential native vegetation is dominated by
stratum is pale brown clay loam. Shale is at a depth of western wheatgrass and blue grams. Buffalograss is also
about 29 inches. present Potential production ranges from 1,000 pounds
Permeability is slow. Available water capacity is per acre in favorable years to 600 pounds in unfavorable
moderate. The effective rooting depth is 20 to 40 inches. years. As range condition deteriorates, a blue grams-buf-
Surface runoff is medium to rapid, and the erosion hazard falograss sod forms. Undesirable weeds and annuals in-
is moderate. vade the site as range condition becomes poorer.
This soil is suited to limited cropping. Intensive Management of vegetation on this soil should be based
cropping is hazardous because of erosion.- The cropping on taking half and leaving half of the total annual produc-
system should be limited to such close grown crops as al- tion. Range pitting can reduce runoff.Seeding is desirable
Calla, wheat, and barley. The soil also is suited to fir- if the range is in poor condition. Western wheatgrass,
rigated pasture. A suitable cropping system is 3 to 4 blue grama, sideoats grams, buffalograss, pubescent
years of alfalfa followed by 2 years of corn and small wheatgrass, and crested wheatgrass are suitable for seed-
grain and alfalfa seeded with a nurse crop. ing. The grass selected should meet the seasonal require-
ments of livestock It can be seeded into a clean, firm
sorghum stubble, or it can be drilled into a firm prepared
seedbed. Seeding early in spring has proven most success-
ful.
Windbreaks and environmental plantings are generally
not suited to this soil. Onsite investigation is needed to
determine if plantings are feasible. Supplemental water is
needed for successful plantings.
Wildlife is an important secondary use of this soil. The
cropland areas provide favorable habitat for ring-necked
pheasant and mourning dove. Many nongame species can
be attracted by establishing areas for nesting and escape
cover. For pheasants, undisturbed nesting cover is essen-
tial and should be included in plans for habitat develop-
ment, especially in areas of intensive agriculture. Range-
land wildlife, for example, the pronghorn antelope, can be
attracted by developing livestock watering facilities,
managing livestock grazing,and reseeding where needed.
This soil has poor potential for urban and recreational
development. The chief limiting features are the underly-
ing shale, the low strength, and the moderate to high
shrink swell. These features present severe problems in
dwelling and road construction and in use of septic tank
absorption fields and sewage lagoons. Capability subclass
IVe irrigated, Vie nonirrigated;Clayey Plains range site.
USDA SOIL CONSERVATION SERVICE
SOIL GROUP DESCRIPTION
RENOHILL SERIES
REFERENCES
1. Colton R.B. and Harold R. Fitch, 1974, Map Showing Potential Sources of Gravel
and Crushed-Rock Aggregate, in the Boulder-Fort Collins-Greeley Area. Front
Range Urban Corridor, Colorado: U.S. Geological Survey Miscellaneous
Investigation Series Map I-855-D.
2. Colton R.B., Holligan, J.A., and Anderson, L.W., 1975, Preliminary Map of
Landslide Deposits, Greeley 1°x2° Quadranele, Colorado: U.S. Geological Survey
Miscellaneous Investigation Series Map MF-704.
3. McCain, J. and Hotchkiss, W.R., 1975, Map Showing Flood-Prone Areas, Boulder-
Fort Collins-Greeley Area,Front Range Urban Corridor, Colorado: U.S. Geological
Survey Miscellaneous Investigation Series Map I-855-E.
4. Colton R.B., 1978, Geologic Map of the Boulder-Fort Collins-Greeley Area,
Colorado: U.S. Geological Survey Miscellaneous Investigation Series Map I-955-G.
5. Hershey L.A. and Schneider, Jr. P.A., 1972, Geologic Map of the Lower Cache La
Poudre River Basin.North-Central Colorado: U.S. Geological Survey Miscellaneous
Investigation Series Map I-687.
6. Hillier D. and Schneider,Jr. P.A., 1979, Depth to the Water Table in the Boulder-Fort
Collins-Greeley Area, Front Range Urban Corridor. Colorado: U.S. Geological
Survey Miscellaneous Investigation Series Map I-855-I.
7. United States Department of Agriculture Soil Conservation Service and Forest
Service in Cooperation with Colorado Agricultural Experiment Station, 1980, Soil
Survey of Weld County Area, Colorado, Maps 239-812/3.
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