Named from Eagles House crags, sec.13 T18N R30E, Lahontan Mountains, Churchill Co, NV, designated as type locality. Also exposed in White Throne Mountains, Desert Mountains, and Eetza Mountain. At type consists of two flows: lower (about 200 ft thick) is pale-greenish-gray porphyritic dacite, and upper (nearly 100 ft thick) is pink porphyritic rhyolite. Rhyolite is faulted against Truckee formation, which locally lies in depositional contact on rhyolite. Unconformably overlies dacite of Rainbow Mountains. Age is considered to be late Miocene to early Pliocene based on stratigraphic relations with Truckee formation.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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