Named for exposures in area drained by Kulthieth, Kaliakh, and Duktoth Rivers, Type locality designated as measured section in vicinity of small lake at head of northeasternmost branch of Kulthieth River, Robinson Mountains, Yakataga district, southern AK. Consists of nonmarine and marine sandstone and siltstone with intercalated thin beds of high-rank coal. At type locality includes three predominantly sandy units which alternate with three predominantly silty units. Total thickness is at least 9300 ft. Base not seen. Apparently conformably underlies Poul Creek formation. Marine invertebrate fossils collected in upper part have been identified by H.E. Vokes as of late Eocene age. Age of Kulthieth formation given as Paleocene(?) and Eocene in map legend.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Kulthieth Formation geographically extended into Bering River area at expense of Kushtaka Formation (thereby abandoning Kushtaka Formation owing to more widespread extent of Kulthieth and equivalent age and lithology of these two units. Consists of interbedded arkosic sandstone, carbonaceous siltstone and shale, with minor coal. In Chugach National Forest overlies Stillwater Formation; underlies Tokun Formation. Age in Chugach National Forest is Eocene only based on fossil plants (Wolfe, 1977; Turner and others, in press) and mollusks (F.S. MacNeil IN Wolfe, 1977) and on stratigraphic relations with underlying and overlying formations. [Overall age remains Paleocene, Eocene, and Oligocene.]
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Age of Kulthieth Formation is early Eocene to early Oligocene based on foraminifers, mollusks, and plant leaves. [Shown on correlation chart of central part of Yakutat terrane, fig.6, p.245].
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Age of Kulthieth Formation is revised to Eocene on the basis of fossils.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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