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Pyroclastic ejecta of basaltic cinder cones (lower Pliocene? and Miocene?)

Mostly unconsolidated, oxidized, fine to course, scoriaceous cinders, bombs, and agglutinate deposited in subaerial environment
StateOregon
NamePyroclastic ejecta of basaltic cinder cones (lower Pliocene? and Miocene?)
Geologic ageMiocene to Early Pliocene
Original map labelTp
Primary rock typebasalt
Secondary rock typeandesite
Other rock types
Lithologic constituents
Major
Igneous > Volcanic > Mafic-volcanic > Basalt (Pyroclastic)Also contains andesite
Minor
Igneous > Volcanic > Mafic-volcanic > Andesite (Pyroclastic, air fall)
Igneous > Volcanic > Mafic-volcanic > Basalt (Pyroclastic, air fall)
Igneous > Volcanic > Mafic-volcanic > Andesite (Pyroclastic)
Map references
Walker, G.W. and MacLeod, N.S., 1991, Geologic map of Oregon: U.S. Geological Survey, scale 1:500,000.
Unit references
Walker, G.W. and MacLeod, N.S., 1991, Geologic map of Oregon: U.S. Geological Survey, scale 1:500,000.
Walker, G.W., 1977, Geologic map of Oregon east of the 121st meridian: U.S. Geological Survey Miscellaneous Geologic Investigations Map I-902, scale 1:500,000.
Swisher, C.C., Ach, J.A., and Hart, W.K., 1990, Laser fusion 40Ar/39Ar dating of the type Steens Mountain Basalt, southeastern Oregon, and the age of the Steens aeromagnetic polarity transition [abs.]: EOS, Transactions of American Geophysical Union, v. 17, no. 43, p. 1,296.
Beeson, J.H., Geology of the southern half of the Huntington quadrangle, Oregon: Eugene, University of Oregon, master's thesis, 77 p.
Geographic coverageBaker - Crook - Harney - Klamath - Lake - Linn - Malheur - Wasco

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