1. Home
  2. Items
  3. Geology and hydrogeology of the Albion Basin, Cassia County, Idaho...
PDF

Geology and hydrogeology of the Albion Basin, Cassia County, Idaho Item Info

Albion basin is an alluvium-filled basin in eastern Cassia County, Idaho, about 18 miles southeast of Burley. The study area is in the Basin and Range province of the western United States. The eastern boundary of the basin is formed by the Malta Range, a rotated fault block which apparently is bounded by high-angle normal faults on the east and west. A line of hot springs marks the probable position of the fault on the west side of the Malta Range. East Hills bounds the basin on the north and the main mass of Albion Range forms the south and west boundaries. The Malta Range and part of the East Hills are made up of a thick flow of quartz latite. The flow consists of three zones: lower and upper vitrophyre zones, and a central lithoidal zone. No mineralogical differences and no physical breaks were noted between the zones. Capping the Malta Ridge in the north is a body of Snake River basalt about one square mile in area. The Albion Rage is underlain by metamorphic rocks. Marsh Creek is the principal stream in the basin, but the ground water is the main source of irrigation and domestic water. Wells range in depth from 11 feet to more than 700 feet and yields range from a few gallons per minute to 540 gallons per minute. Wells must be cased the entire depth of penetration. Several clay lenses in the alluvium create local artesian aquifers. The water, mostly of the calcium-bicarbonate type, is suitable for domestic and irrigation use: the total dissolved solids content ranges from 202 ppm. to 2294 ppm; temperatures of the waters in the deep wells are generally 62 degrees to 74 degrees Fahrenheit, and in the shallow wells, 57 degrees Fahrenheit. Hot springs in Marsh Canyon are used only for irrigation, although the possibility exists that they could be developed for domestic heating or for recreation. Quantitative data on water resources could not be obtained from the present study, but available data suggest that the basin is not yet fully developed.

View on Timeline View on Map Download PDF
Title:
Geology and hydrogeology of the Albion Basin, Cassia County, Idaho
Authors:
Myers, David Arthur
Date Created (ISO Standard):
1967-05
Description:
Albion basin is an alluvium-filled basin in eastern Cassia County, Idaho, about 18 miles southeast of Burley. The study area is in the Basin and Range province of the western United States. The eastern boundary of the basin is formed by the Malta Range, a rotated fault block which apparently is bounded by high-angle normal faults on the east and west. A line of hot springs marks the probable position of the fault on the west side of the Malta Range. East Hills bounds the basin on the north and the main mass of Albion Range forms the south and west boundaries. The Malta Range and part of the East Hills are made up of a thick flow of quartz latite. The flow consists of three zones: lower and upper vitrophyre zones, and a central lithoidal zone. No mineralogical differences and no physical breaks were noted between the zones. Capping the Malta Ridge in the north is a body of Snake River basalt about one square mile in area. The Albion Rage is underlain by metamorphic rocks. Marsh Creek is the principal stream in the basin, but the ground water is the main source of irrigation and domestic water. Wells range in depth from 11 feet to more than 700 feet and yields range from a few gallons per minute to 540 gallons per minute. Wells must be cased the entire depth of penetration. Several clay lenses in the alluvium create local artesian aquifers. The water, mostly of the calcium-bicarbonate type, is suitable for domestic and irrigation use: the total dissolved solids content ranges from 202 ppm. to 2294 ppm; temperatures of the waters in the deep wells are generally 62 degrees to 74 degrees Fahrenheit, and in the shallow wells, 57 degrees Fahrenheit. Hot springs in Marsh Canyon are used only for irrigation, although the possibility exists that they could be developed for domestic heating or for recreation. Quantitative data on water resources could not be obtained from the present study, but available data suggest that the basin is not yet fully developed.
Subjects:
geology geohydrology Cassia County
Location:
Snake River
Latitude:
42.41
Longitude:
-113.57
Collection:
Boise Basin
Series:
Water for Idaho
IWRRI number:
196704
Rights:
In copyright, educational use permitted. Educational use includes non-commercial reproduction of text and images in materials for teaching and research purposes. For other contexts beyond fair use, including digital reproduction, please contact the University of Idaho Library Special Collections and Archives Department at libspec@uidaho.edu. The University of Idaho Library is not liable for any violations of the law by users.
Publisher:
University of Idaho
Contributing Institution:
University of Idaho
Type:
Text
Format:
application/pdf
Cataloger:
Jodi Haire
Date Digitized:
2008-09-18

Contact us about this record

Source
Preferred Citation:
"Geology and hydrogeology of the Albion Basin, Cassia County, Idaho", Idaho Waters Digital Library, University of Idaho Library Digital Collections, https://www.lib.uidaho.edu/digital/iwdl/items/iwdl-196704.html
Rights
Rights:
In copyright, educational use permitted. Educational use includes non-commercial reproduction of text and images in materials for teaching and research purposes. For other contexts beyond fair use, including digital reproduction, please contact the University of Idaho Library Special Collections and Archives Department at libspec@uidaho.edu. The University of Idaho Library is not liable for any violations of the law by users.
Standardized Rights:
http://rightsstatements.org/vocab/InC-EDU/1.0/
« Previous Back to Browse Next »