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- W2023761443 abstract "The known igneous history of southwestern Idaho began with the deposition of a great thickness of Permian andesites and rhyolite. Following this in Jurassic (?) time occurred the intrusion of the Idaho batholith. After an extensive erosion interval followed the extrusion of the lower series of Columbia River basalt. During a period of quiescence the Payette formation was deposited. This was followed by the extrusion of the upper series of the Columbia River basalt upon which was developed a peneplain-like erosion surface. Before the deposition of the Idaho formation the Owyhee rhyolite was extruded, which is part of a widespread sheet of acidic lavas which extends over southern Idaho and parts of adjacent states. Probably contemporaneous with these acid flows occurred the intrusion of one or more small batholiths into the Payette formation and Columbia River basalt. Down-warping was initiated, and upon the upper series of the Columbia River basalt and the Owyhee rhyolite was deposited the Idaho formation in Pliocene time. The Snake River basalt was extruded into the downwarp to the east in Pliocene and chiefly Pleistocene time, and it encroached on the Idaho formation in southwestern Idaho in the Pleistocene." @default.
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- W2023761443 date "1931-08-01" @default.
- W2023761443 modified "2023-09-24" @default.
- W2023761443 title "Igneous Geology of Southwestern Idaho" @default.
- W2023761443 doi "https://doi.org/10.1086/623879" @default.
- W2023761443 hasPublicationYear "1931" @default.
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