Pg. C30-C34. Fitz Creek Siltstone, 3rd from lowermost formation (of 6) of Tuxedni Group. Name proposed to replace term siltstone member of former Tuxedni Formation of older reports. Composed mainly of massive bluish-gray arenaceous siltstone that commonly weathers rusty brown and contains many small fossiliferous limestone concretions, interbedded fine-grained sandstone and, locally, conglomerate. Thickness 1,090 feet at type locality. Conformably overlies Gaikema Sandstone; conformably underlies Cynthia Falls Sandstone (both of Tuxedni Group). Age is Middle Jurassic (Bajocian).
Type locality: on Tonnie Creek, a tributary of Fitz Creek, starting 7,000 ft S. 55 deg. E. of Tonnie Peak and continuing upstream for 1,400 ft. Named from Fitz Creek, a principal stream on Iniskin Peninsula, Cook Inlet region, southeastern AK.
Source: US geologic names lexicon (USGS Bull. 1350, p. 259); supplemental information from GNU records (USGS DDS-6; Menlo GNULEX).
Pg. 29-31, pls. Fitz Creek Siltstone. On Iniskin Peninsula, outcrops [on] Tonnie syncline. These belts, 1,000-1,500 feet wide, lie between two prominent hogback ridges on lower slopes of mountain mass formed by Tonnie syncline. The hogback ridges are formed by sandstone and conglomerate of the underlying Gaikema and overlying Cynthia Falls Sandstones. Thickness 650 to 1,280 feet.
Source: US geologic names lexicon (USGS Bull. 1350, p. 259).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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