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Publications

The following is a list of our publications available from the USGS Publications Warehouse. If you cannot find what you are looking for, please contact our Public Information Officer, Tim Merrick, at trmerrick@usgs.gov or 208-387-1305.

Filter Total Items: 463

An evaluation of water-quality data obtained at four streamflow daily-record stations in Idaho An evaluation of water-quality data obtained at four streamflow daily-record stations in Idaho

Chemical data for four stream-gaging stations in Idaho, each having 6 to 22 years of available records, were analyzed to determine functional relations between concentrations of the major inorganic constituents, specific conductance, and stream discharge. Three of the four stations had sufficient available record for assessing changes in constituent relations with time. The records for...
Authors
Kenneth L. Dyer

A proposed streamflow-data program for Idaho A proposed streamflow-data program for Idaho

A streamflow information system is proposed for Idaho. This proposal resulted from a study in which the basic steps were (1) definition of long-term program goals, (2) examination and evaluation of available data to determine which goals have been achieved, and (3) consideration of alternate programs and techniques for meeting the remaining goals. The following conclusions are drawn from...
Authors
C.A. Thomas, W. A. Harenberg

Water resources in the Big Lost River Basin, south-central Idaho Water resources in the Big Lost River Basin, south-central Idaho

The Big Lost River basin occupies about 1,400 square miles in south-central Idaho and drains to the Snake River Plain. The economy in the area is based on irrigation agriculture and stockraising. The basin is underlain by a diverse-assemblage of rocks which range, in age from Precambrian to Holocene. The assemblage is divided into five groups on the basis of their hydrologic...
Authors
E. G. Crosthwaite, C.A. Thomas, K.L. Dyer

Availability of ground water for large-scale use in the Malad Valley-Bear River areas of southeastern Idaho: an initial assessment Availability of ground water for large-scale use in the Malad Valley-Bear River areas of southeastern Idaho: an initial assessment

Five areas within the Bear River drainage of southeastern Idaho offer potential for further development of ground water--the valley north of Bear Lake, north of Soda Springs, Gem Valley, Cache Valley in Idaho, and Malad Valley in Idaho. Saturated deposits north of Bear Lake are too fine-textured to yield large quantities to wells; the areas north of Soda Springs and in Gem Valley would...
Authors
W.L. Burnham, A.H. Harder, N. P. Dion

Optical method for determining particle sizes of coarse sediment Optical method for determining particle sizes of coarse sediment

A particle-size analyzer was used to determine particle sizes of sediment by an optical technique based on an adjustable circle of light which determines the intermediate axis of the sediment particles shown on a photograph. Data from counting particles in various size ranges can be presented either in the form of a particle count or volumetric analysis. Comparison with standard methods...
Authors
John R. Ritter, Edward J. Helley

Water resources of the Salmon Falls Creek basin, Idaho-Nevada Water resources of the Salmon Falls Creek basin, Idaho-Nevada

The northern part of the Salmon Falls Creek basin, referred to as the Salmon Falls tract, contains a large acreage of good agricultural land, but the surface-water supply is inadequate to develop the area fully. Attempts to develop ground water for irrigation have been successful only locally. Specific capacities of wells drilled for irrigation and for test purposes ranged from less than...
Authors
E. G. Crosthwaite

Ground-water aspects of the lower Henrys Fork region, Idaho Ground-water aspects of the lower Henrys Fork region, Idaho

The lower Henrys Fork region includes the plains and low benches between Ashton and the junction of Henrys Fork and Snake River in eastern Idaho. The northwestern and western parts of the area are part of the Snake River lava plain. The central part of the area is occupied by alluvial plains of the Snake, Teton, and Falls Rivers, and Henrys Fork. The southeastern part of the area is a...
Authors
E.J. Crosthwaite, M.J. Mundorff, E.H. Walker
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