My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WSP05281
CWCB
>
Water Supply Protection
>
Backfile
>
5001-6000
>
WSP05281
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 2:17:40 PM
Creation date
10/12/2006 12:56:59 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.145.A
Description
La Plata Project (New Mexico)
Basin
San Juan/Dolores
Date
11/24/1941
Author
USDOI/BOR
Title
La Plata Project: Colorado-New Mexico - Project Investigations Report No. 32
Water Supply Pro - Doc Type
Report/Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
71
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />..... <br />.... <br />~. <br />- <br /> <br />C'.'" <br /> <br />.";> <br /> <br />The soils of Red Mesa and Fort Lewis Mesa which together <br /> <br />constitute the main body of the project area in Colorado are <br /> <br />described by Associate Engineer H. F. Bahmeier as follows: <br /> <br />The soil is a reddish sandy loam to loam, of good depth and <br /> <br />underlaid with gravel. A well defined slightly compacted lime <br /> <br />zone usually about one foot in thickness is encountered at <br /> <br />from 36 to 42 inches from the surface. This layer is either <br /> <br />underlaid directly by gravel or by loose sandy loam which <br /> <br />gives way to gravel at greater depths. <br /> <br />The drainage is excellent but at the same time the lime <br /> <br />layer provides enough temporary impediment to percolating <br /> <br />water so that irrigation ~~ter can be distributed over the <br /> <br />fields with little loss due to deep percolation. The soil was <br /> <br />found to be shallow and sometimes rocky near the borders of <br /> <br />the mesa, particularly where points were left by the erosion <br /> <br />of side draws. Over the remainder of the mesa, however, the <br /> <br />soil was found to be practically all class 1, the larger per- <br /> <br />centage of class 2 being accounted for by the fact that the <br /> <br />it <br />~ <br /> <br />topography was not sufficiently smooth for class 1. . <br /> <br />~. <br />, <br /> <br />., <br /> <br />::. <br /> <br />11 <br /> <br />".,1 <br />
The URL can be used to link to this page
Your browser does not support the video tag.