My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
7086
CWCB
>
UCREFRP
>
Copyright
>
7086
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/11/2009 11:06:54 AM
Creation date
8/10/2009 12:35:04 PM
Metadata
Fields
Template:
UCREFRP
UCREFRP Catalog Number
7086
Author
U.S. Fish and Wildlife Service.
Title
Indexed, Annotated Bibliography of the Endangered and Threatened Fishes of the Upper Colorado River System.
USFW Year
1977.
USFW - Doc Type
Denver, Co.
Copyright Material
YES
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
173
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
60. Bjorklund, L. J. 1969. Reconnaissance of the HYDROLOGY <br />ground-water of the upper Fremont River WATER QUAL. <br />valley, Wayne County, Utah. Utah Department TEMPERATURE <br />of Natural Resources, Salt Lake City. WATER QUAN. <br />Technical Publications No. 22. 54 pp. <br />The drainage basin for the Fremont River valley <br />includes about 700 square acres. The source of <br />most of the ground water is precipitation on <br />the Fish Lake, Awapa, and Aquarius plateaus, <br />where annual precipitation is between 20-40 <br />inches. A large but undetermined quantity of <br />water is stored under both artesian and water <br />table conditions in volcanic rocks bordering <br />and underlying the valley. More than one <br />million acre feet is stored in the unconsolidated <br />valley fill. The principle phreatophytes in <br />this area are meadow grass, rabbitbrush, and <br />greasewood which grows in fringe areas. Ground <br />water is used primarily in agriculture and to <br />supply Fremont, Loa, Lyman, and Bicknell, also <br />for domestic use, stock use, and fish culture. <br />Water has a low sodium content,-some have high <br />salinity, none of the maximum concentrations of <br />dissolved constituents recommended for drinking <br />water were exceeded in samples collected. -The <br />temperature of ground water ranged from 47° to <br />63° F. <br />61. Blackman, W. C., Jr., J. V. Rouse, G. R. <br />Schillinger, and W. H. Shafer, Jr. 1973. <br />Mineral pollution in the Colorado River <br />basin. Journal Water Pollution Control <br />Federation 45(7):1717-1557. <br />The Colorado River Basin Water Quality Control <br />Project has carried out extensive field investiga- <br />tions to determine the location, magnitude, and <br />causes of interstate water pollution problems. <br />This paper summarizes the methodology and <br />findings of the review of existing mineral <br />quality data and the evaluation of .salinity <br />sources. (Wydoski) <br />HYDROLOGY <br />POLLUTION <br />SALINITY <br />SEDIMENT <br />WATER QUAL. <br />COLORADO R. <br />62. Bolke, E. L. 1976. Chemical and physical data DATA <br />for the Flaming Gorge Reservoir area, Utah WATER QUAL. <br />and Wyoming, 1973-1975. U. S. Geologic RESERVOIR <br />Survey, Salt Lake City, Utah. U. S. TEMPERATURE <br />Geological Survey, Open-file Report. FLAMING GORGE RES. <br />Basic Data Release No. 27. 35 pp. <br />35 <br />
The URL can be used to link to this page
Your browser does not support the video tag.