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WSP05425
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Last modified
1/26/2010 2:18:18 PM
Creation date
10/12/2006 1:01:19 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8101
Description
Arkansas River Basin Description
State
CO
Basin
Arkansas
Water Division
2
Date
9/1/1962
Author
High Plains SCD
Title
Watershed Work Plan - Limon Watershed Protection Project - Elbert and Lincoln Counties - Colorado
Water Supply Pro - Doc Type
Report/Study
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<br />~ <br /> <br />I <br /> <br />O~1745 <br /> <br />I <br /> <br />- 5 - <br /> <br />I <br /> <br />The upper part of the West drainage contains relatively steep <br />slopes and is dissected by numerous deep ravines, The remainder of <br />the watershed above the Town of LUuon generally has a broadly rolling <br />topography. The major streams draining this area occupy broad, <br />grassed floodplains that range from 500 to 1,000 feet in width, The <br />stream channels are incised from 5 to 10 feet below the general <br />floodplain surface and are usually narrow with grassed banks and <br />beds. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />In the lower part of the watershed, the floodplains of the three <br />tributary streams join to form a broad, gently sloping alluvial <br />plain on which most of the Town of Limon is located. This plain <br />occupies a low terrace position in relation to Big Sandy Creek. <br /> <br />I <br /> <br />Soils.- The principal soils in the upper one-third of the <br />watershed are those developed on sandy shales of the Fox Hills <br />and Pierre formations. These soils are predominantly sandy clay <br />loams and are shallow to moderately deep, Internal drainage is <br />slow to moderate, Small areas of very fine sandy loam and some areas <br />of rough gullied land are present at the extreme upper end, <br /> <br />I <br /> <br />I <br /> <br />The lower two-thirds of the watershed contains extensive <br />areas of soils developed on eolian and alluvial materials as well <br />as soils developed on shales of the Pierre formation, The eolian <br />materials have a high percentage of silt and the soils are primarily <br />loams. Water intake is generally good, Soils on alluvial materials <br />and on shale are predominantly clay and clay loam and some are high <br />in alkaline salts. The intake of water is usually slow on these <br />soils, <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Range Sites.- The principal kinds of rangelands and the approximate <br />percentages of each are: Clayey Plains range site (45 percent); <br />Loamy Plains range site (25 percent); Loamy Slopes range site (15 <br />percent); and Breaks range site (15 percent), Range condition was <br />determined by comparing the present vegetation on each range site <br />with the potential vegetation that the site can grow, The major <br />portion of the area (about 85 percent) was found to be in good <br />condition. The condition of the remaining 15 percent ranged from <br />poor to excellent" Approximately 2,500 acres of the Clayey <br />Plains and Loamy Slopes areas have been contour-furro,,,,d. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />~~ <br />
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