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WSP08184
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Last modified
1/26/2010 2:30:27 PM
Creation date
10/12/2006 2:47:43 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8200.765
Description
White River General
State
CO
Basin
Yampa/White
Water Division
6
Date
11/1/1966
Author
USFS
Title
Water and Related Land Resources - White River Basin in Colorado
Water Supply Pro - Doc Type
Report/Study
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<br />I <br /> <br />The unit encompasses steep slopes, canyons, and rocky ledges bordering <br />the White River and tributary intermittent streams. The deeply cut, <br />narrow drainageways are separated at frequent intervals by higher <br />lying uplands and mesas. Shale outcrops and badlands oCGUPY many <br />lower slopes. Slope gradients are generally 10 to 70 percent but <br />gradients of less than 5 percent are common on alluvial fans, bottom- <br />lands and mesas. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Most of unit 2 is at an elevation of between 5,200 and 6,200 feet. <br />Climate in this unit is somewhat similar to that at Range1y with a <br />mean annual precipitation estimated at 8 to 12 inches. Mean annual <br />temperature is about 470 F. and the frost-free period is from 90 to <br />l24 days. <br /> <br />I <br /> <br />Soil parent materials are primarily sandstones and <br />material from residual beds. Gravelly, calcareous <br />eolian deposits cap mesas and some upland ridges. <br />recent alluvium are of minor extent. <br /> <br />shales or reworked <br />outwash, and local <br />Soils forming in <br /> <br />I <br /> <br />I <br /> <br />Surface soils are light colored, thin and usually calcareous. Unit 2 <br />has more stony surface soils and associated rock outcrop than are present <br />in unit 1. Conspicuous rock ledges along Raven Ridge northwest of <br />Rangely, are representative. Surface textures of soils forming from <br />sandstone are usually stony or gravelly sandy loarns while clay and <br />clay loam textures are common for shale derived soils. Subsoils range <br />from sandy loam to clay in texture. Over most of the area, underlying <br />sandstone or shale beds are within 20 inches of the surface and plant <br />rooting depths are restricted. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Composition of unit 2 by Great Soil Groups, except for Regosols that <br />are included with the zonal soils and land types, is estimated as <br />follows: <br /> <br />I <br /> <br />Percent <br /> <br />1949 Great Soil Group <br /> <br />1965 Great Group, Subgroup <br />or Family <br /> <br />Haplorthents <br />(Lithic 30%) <br />(Thin 30%) <br /> <br />I <br /> <br />60 <br /> <br />Lithosols <br />(Sandstone 30%) <br />(Shale 30%) <br /> <br />I <br /> <br />25 <br /> <br />Desert and Sierozem soils <br /> <br />Haplargids and Camborthids <br /> <br />I <br /> <br />5 <br /> <br />Alluvial soils <br /> <br />Haplorthents <br /> <br />10 <br /> <br />.Land types <br />(Rock outcrop 5%) <br />(Shale badlands 5%) <br /> <br />Land types <br />(Rock outcrop 5%) <br />(Shale badlands 5%) <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />- l6 - <br /> <br />I <br />
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