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Geologic units in Lincoln county, Idaho

[Additional scientific data in this geographic area]

Basalt, gravel, and pumice; Late Pleistocene basaltic volcanics and interlayered sedimetnsof subunit 3b; Snake River Plain (Late Pleistocene) at surface, covers 6 % of this area
Upper Pleistocene Snake Plain basaltic lava flows, unit 3.
Lithology: tholeiite; lava flow; gravel; pumice
Gravel, sand, and silt; Quaternary; alluvium (Quaternary) at surface, covers 0.6 % of this area
Quaternary alluvium; may contain some glacial deposits and colluvium in uplands
Lithology: alluvium; alluvial terrace; floodplain; alluvial fan; colluvium
Basalt flows, basaltic pyroclastic and clastic debris; Middle Pleistocene canyon-filling and plateau lava flows, pyroclastic debris, alluvium, and colluvium; Snake River Plain (Middle Pleistocene) at surface, covers 13 % of this area
Middle Pleistocene plateau and canyon-filling basalt in and near Snake Plain.
Lithology: tholeiite; lava flow; pyroclastic; alluvium; colluvium
Basalt, clay, and pumice; Late Pleistocene basalt flows, volcaniclastic debris, and ponded sediments of subunit 4b; Snake River Plain; (Late Pleistocene) at surface, covers 31 % of this area
Upper Pleistocene Snake Plain basaltic lava flows, unit 4.
Lithology: tholeiite; lava flow; clay or mud; pumice
Basalt and gravel; Late Pleistocene basalt flows and interlayered gravel of subunit 2b; Snake River Plain (Late Pleistocene) at surface, covers 16 % of this area
Upper Pleistocene Snake Plain basaltic lava flows, unit 2.
Lithology: tholeiite; lava flow; gravel
Basalt, pumice; Holocene basaltic lava flows and cinder cones; Snake River Plain and vicinity (Holocene) at surface, covers 11 % of this area
Recent, relatively unweathered Snake Plain basalt flows and cinder cones.
Lithology: tholeiite; lava flow; pumice
Basalt, clay, and gravel; Late Pleistocene basalt flows with interlayered alluvial and lacustrine sediments; Snake River Plain and vicinity (subunits are Qpu1b, Qpu2b, Qpu3b, and Qpu4b) (Late Pleistocene) at surface, covers 6 % of this area
Upper Pleistocene Snake Plain lava flows; local stratigraphic position shown by (Qpu4b, Qpu3b, Qpu2b, Qpu1b).
Lithology: tholeiite; lava flow; clay or mud; gravel
Surficial sediments; Quaternary alluvial, lacustrine, eolian, and glacial-outwash deposits, undivided; Snake River Plain, and Basin-and-Range provinces (Quaternary) at surface, covers 0.3 % of this area
Quaternary surficial cover; Snake Plain stream, lake, wind and glacial-flood mantle.
Lithology: loess; colluvium
Basalt flows, pyroclastic debris, clastic sediments, and diatomite; Pliocene basaltic volcanics and clastic sediments; Snake River Plain and vicinity (Pliocene) at surface, covers 0.1 % of this area
Pliocene olivine basalt flows and associated tuff and detritus of southern Idaho.
Lithology: basalt; lava flow; tuff; mixed clastic/volcanic
Basalt flows, pumice, and tuff; Early Pleistocene to Pliocene basaltic volcanics; Snake River Plain (Early Pleistocene) at surface, covers 6 % of this area
Lower Pleistocene to Pliocene basalts with associated tuffs and volcanic detritus.
Lithology: tholeiite; lava flow; pumice; tuff
Rhyolite, quartz latite, and latite ignimbrites and flows; Miocene felsic volcanics; Owyhee Plateau; (Miocene) at surface, covers 4 % of this area
Miocene silicic flows, tuffs; most common in southwestern Idaho.
Lithology: rhyolite; latite; quartz latite; ignimbrite; lava flow
Basalt and silt; Late Pleistocene basalt flows and interlayered lacustrine silt beds of subunit 1b; Snake River Plain (Late Pleistocene) at surface, covers 5 % of this area
Upper Pleistocene Snake Plain basaltic lava flows, unit 1.
Lithology: tholeiite; lava flow; silt

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