
Volcanic geology dominates the landscape of southern Idaho along the border of Minidoka and Blaine Counties during the early 1970s. The terrain is defined by extensive Lava flows and unique geological formations, most notably the Bear Trap Lava Tube in the northeastern section and the prominent rise of Whiskey Butte. This arid environment is marked by an intricate system of ephemeral water sources and catchments, including Big Sinks Reservoir, Gabettas Reservoir, and Antelope Reservoir.
24 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1954 · Pocatello
USGS Topo · 1:250,000
1955 · Idaho Falls
USGS Topo · 1:250,000
1958 · Idaho Falls
USGS Topo · 1:250,000
1958 · Pocatello
USGS Topo · 1:250,000
1972 · Schodde Well
USGS Topo · 1:24,000
1972 · Bear Trap Cave
USGS Topo · 1:24,000
1972 · Mule Butte
USGS Topo · 1:24,000
1972 · Bear Park SW
USGS Topo · 1:24,000
1972 · Minidoka
USGS Topo · 1:24,000
1972 · Max
USGS Topo · 1:24,000