Named for exposures near mining district of Turnagain Arm and vicinity of which Sunrise City is center, southern AK. Outcrops on western shores of Prince William Sound. May make up Kenai Mountains which occupy two-thirds of peninsula. Consists of metamorphic gold-bearing rocks of interbedded, fine blue-black slates and dark-gray arkoses. Intruded by series of dikes, chiefly aplitic in character. No fossils were found. Tentatively assigned late Paleozoic age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
"Sunrise series" of Mendenhall (1900) is at least westward or southwestward continuation of rocks recognized by later geologists as Valdez group. "Sunrise series" is not used as an additional stratigraphic name in this paper. [Thus "Sunrise series" is abandoned]. Fragment and imprints of INOCERAMUS collected from "Sunrise group" (Park, 1933, USGS Bull. 849, p.393-394) indicate age is Late Cretaceous.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
["Sunrise series"] of Moffit (1954) is redescribed as Sunrise Group. Described as thick turbidite suite now extensively exposed in geanticlinal welt of Kenai-Chugach Mountains. Age given as Cretaceous in correlation chart of Cook Inlet basin.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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