scholarly journals Groundwater-quality data from the eastern Snake River Plain Aquifer, Jerome and Gooding Counties, south-central Idaho, 2017

Data Series ◽  
2018 ◽  
Author(s):  
Kenneth D. Skinner
Keyword(s):  
Groundwater Quality ◽  
Snake River Plain ◽  
Quality Data ◽  
Snake River ◽  
South Central ◽  
River Plain ◽  
Central Idaho

Age of Irrigation Water in Ground Water from the Eastern Snake River Plain Aquifer, South-Central Idaho

Ground Water ◽  
2000 ◽  
Vol 38 (2) ◽  
pp. 264-283 ◽  
Author(s):  
L.N. Plummer ◽  
M.G. Rupert ◽  
E. Busenberg ◽  
P. Schlosser
Keyword(s):  
Ground Water ◽  
Irrigation Water ◽  
Snake River Plain ◽  
Snake River ◽  
South Central ◽  
River Plain ◽  
Central Idaho

The geology of split butte — A maar of the south-central snake river plain, Idaho

1980 ◽  
Vol 43 (3) ◽  
pp. 453-471 ◽  
Author(s):  
M. B. Womer ◽  
R. Greely ◽  
J. S. King
Keyword(s):  
Snake River Plain ◽  
Snake River ◽  
The South ◽  
South Central ◽  
River Plain

Calcareous algae and associated microfossils from Mid-Carboniferous rocks in east-central Idaho

1986 ◽  
Vol 60 (2) ◽  
pp. 476-496 ◽  
Author(s):  
John R. Groves
Keyword(s):  
Snake River Plain ◽  
Calcareous Algae ◽  
Snake River ◽  
East Central ◽  
Genus Level ◽  
Upper Paleozoic ◽  
Biostratigraphic Correlation ◽  
River Plain ◽  
Central Idaho

Mid-Carboniferous (upper Chesterian–lower Atokan) rocks exposed north of the Snake River Plain in east-central Idaho are assigned to the Arco Hills, Bluebird Mountain and lower Snaky Canyon formations (ascending order). In the southern Lemhi Range, calcareous algae and associated microproblematica from these rocks include representatives of at least 13 genera and genus-level taxa within the Dasycladaceae, Aoujgaliaceae, Ungdarellaceae, and incertae familiae. Local appearances of Masloviporidium delicata and Donezella lutugini are early Morrowan or younger as determined independently by studies of associated foraminifers and conodonts. Beresella polyramosa and Komia abundans are locally restricted to Atokan rocks. These findings are consistent with compiled data on worldwide stratigraphic distributions of these taxa, and suggest that certain Upper Paleozoic calcareous algae may be of limited value in biostratigraphic correlation.

Topographic Distortion of a Cold Front over the Snake River Plain and Central Idaho Mountains

2001 ◽  
Vol 16 (3) ◽  
pp. 301-314 ◽  
Author(s):  
W. James Steenburgh ◽  
Thomas R. Blazek
Keyword(s):  
Cold Front ◽  
Snake River Plain ◽  
Snake River ◽  
River Plain ◽  
Central Idaho

Precious Opal Mining in the Snake River Plain Rhyolites, Idaho

1972 ◽  
Vol 13 (3) ◽  
pp. 100-104 ◽  
Author(s):  
Paul L. Broughton
Keyword(s):  
Snake River Plain ◽  
Snake River ◽  
River Plain ◽  
Precious Opal

Distribution, movements and habitats of sage grouseCentrocercus urophasianuson the Upper Snake River Plain of Idaho: changes from the 1950s to the 1990s

2000 ◽  
Vol 6 (1) ◽  
pp. 265-270 ◽  
Author(s):  
Kara M. Leonard ◽  
Kerry P. Reese ◽  
John W. Connelly
Keyword(s):  
Snake River Plain ◽  
Snake River ◽  
The 1950S ◽  
River Plain

Gravity survey in the western Snake River Plain, Idaho-a progress report

1961 ◽  
Author(s):  
David P. Hill ◽  
Jimmy J. Jacobson
Keyword(s):  
Progress Report ◽  
Snake River Plain ◽  
Gravity Survey ◽  
Snake River ◽  
River Plain
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