Effect of irrigation on ground water in southern Canyon County, Idaho
Read Online

Effect of irrigation on ground water in southern Canyon County, Idaho

  • 463 Want to read
  • ·
  • 82 Currently reading

Published by U.S. G.P.O. in Washington, D.C .
Written in English


  • Borings,
  • Irrigation,
  • Water-supply,
  • Groundwater

Book details:

Edition Notes

Statementby P.R. Stevens
SeriesGeological Survey water-supply paper -- 1585
ContributionsUnited States. Bureau of Reclamation
LC ClassificationsTC801 .U2 no. 1585
The Physical Object
Paginationiv, 74 p. :
Number of Pages74
ID Numbers
Open LibraryOL24835047M
LC Control Number62000221

Download Effect of irrigation on ground water in southern Canyon County, Idaho


trees requires more than 40 inches of water during a growing season to remain green and healthy. Add to southwestern Idaho’s climate the fact that it stands face-to-face with limited water resources, and the challenge of maintaining a beautiful landscape in the future becomes quickly evident. Even with sufficient irrigation water, the desertFile Size: KB. The Teton Basin Project was located in eastern Idaho. Teton Dam lay in Fremont County, and was intended to serve agricultural lands of the Fremont-Madison Irrigation District, in Fremont and Madison Counties. The dam sat on the Teton River, a tributary of the Henrys Fork of the Snake River. River from Rupert and Burley west through Canyon County. Limited production of beans can be found without irrigation in the northern counties of Latah, Nez Perce, Clearwater, and Lewis. Southern Idaho counties grow mostly Great Northern, Pinto, and Red Mexican varieties with some Michelite, Cranberry, Kidney, and Sanilac varieties. The depth to the water table can change (rise or fall) depending on the time of year. During the late winter and spring when accumulated snow starts to melt and spring rainfall is plentiful, water on the surface infiltrates into the ground and the water table rises. When water-loving plants start to grow again in the spring and precipitation gives way to hot, dry summers, the.

  Water Well Drilling Information Revised: Septem In the State of Utah, wells regulated by the State Engineer that are drilled to a depth of greater than 30 feet must be constructed by a currently licensed Utah Licensed Well Driller.   Below are descriptions of the basic components found in a private water well. (Source: National Ground Water Association) Well Casing is the tube-shaped structure placed in the well to maintain the well opening from the target ground water to the surface. Along with grout, the casing keeps dirt and excess water out of the well. Complete list of all current permits issued by DEQ, which include permits to regulate emissions of air pollutants, reuse of treated wastewater, and treatment, storage, and disposal of hazardous waste. P.O. Box Boise, ID P: | F:

Today, the city is the largest in Canyon County, is home to alm people and trains are still a large part of the city's landscape. Clark said the location of original water tower the city. Of river water diverted into an earthen irrigation canal system, some was consumed by crop evapotranspiration %, the rest returned to the river as surface return flow % and shallow. Idaho coronavirus updates: 2, total cases, 81 deaths, 2, recovered; Community spread confirmed in Cassia County Boise city leaders considering 2% property tax increase Right Now. The saturated zone beneath the water table is recharged by the excess water that is not discharged to streams. The resulting rise in the water table increases ground-water storage (the volume of ground water stored within an aquifer system). In late spring, summer, and early fall, evaporation and transpiration by plants capture most of the water that would otherwise recharge the aquifer, while.