First use of the Inkom Formation [credited to Crittenden and others (in press?)]. Age is Precambrian.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Pg. 586, 591. Inkom Formation. Present in Pocatello area, Bannock County, southeastern Idaho, and possibly Huntsville area, Weber County, northern Utah. Consists of greenish phyllite that grades upward into greenish-gray to light-olive-gray argillite or slate, siltite, and very fine-grained quartzite. Contains a few beds of conglomerate or impure micaceous quartzite. Thickness at type section 305 m [approx. 1,000 feet]; ranges from 240 to 730 m [approx. 780 to 2,400 feet]. Tentatively assigned to the Brigham Group (revised) in the Huntsville area. Overlies Caddy Canyon Quartzite (new) (only tentatively in Huntsville area); lower contact placed at top of highest quartzite of Caddy Canyon, though some phyllite beds are present below it. Underlies Mutual Formation (extended into Pocatello area); upper contact placed at base of massive quartzite ledges of Mutual. Age is late Precambrian (Precambrian Z). (Inkom Formation adopted by the USGS.)
Type section: north of Portneuf River, in head of small canyon which joins river about a mile (2 km) west of town of Inkom, in northwest part of T. 7 S., R. 36 E., Bannock Co., ID (Northern Rocky Mountain region). Named from town of Inkom.
Source: GNU records (USGS DDS-6; Denver GNULEX, Menlo GNULEX); US geologic names lexicon (USGS Bull. 1520, p. 148-149); Changes in stratigraphic nomenclature, 1971 (USGS Bull. 1372-A, p. A10-A11).
Inkom Formation is definitely included in the Brigham Group in Utah. Age is Precambrian.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Inkom Formation. Extended into the Sheeprock Mountains of north-central Utah (Great Basin region) as 1 of 4 formations of the Brigham Group. Thickness 30 to 145 m. Consists of olive-drab, liver-colored, blue or gray siltstone, shale, and slate, and interbeds of greenish-gray, very fine-grained, ripple-marked sandstone. In northwest part of mapped area, white, medium-grained quartzite is present in upper part. Upper part of the Inkom (this report) = lower argillite member of Cohenour's (1959) Mutual Formation. Overlies Caddy Canyon Quartzite and underlies Mutual Formation (both of Brigham). Age is Late Proterozoic. Report includes geologic map, stratigraphic sections.
Source: Modified from GNU records (USGS DDS-6; Denver GNULEX).
Assigned as 1 of 6 formations to the Brigham Group (group rank extended to southeast ID) in the northern Bannock and Portneuf Ranges and as 1 of 7 formations in the southern Portneuf and Bear River Ranges, Bannock and Bear Lake Cos, ID in the Northern Rocky Mountain region. Overlies Caddy Canyon Quartzite of Brigham; underlies Mutual Formation of Brigham. The lower contact is gradational and the upper contact is disconformable. Is also assigned to depositional sequence 2, a marine sequence. Is one of the most laterally persistent units in the Brigham. Cross section. Late Proterozoic age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Age of the Inkom Formation is revised from Proterozoic Z to Late Proterozoic.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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