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National Geologic Map Database
Geologic Unit: Joe Creek
Map showing publication footprint
  • Usage in publication:
    • Joe Creek Member*
  • Modifications:
    • Named
    • Biostratigraphic dating
  • Dominant lithology:
    • Mudstone
    • Siltstone
    • Limestone
  • AAPG geologic province:
    • Alaska Northern region
Publication:

Detterman, R.L., Reiser, H.N., Brosge, W.P., and Dutro, J.T., Jr., 1975, Post-Carboniferous stratigraphy, northeastern Alaska: U.S. Geological Survey Professional Paper, 886, 46 p.


Summary:

Named as lower member (of 2) of Echooka Formation of Sadlerochit Group for exposures near Joe Creek, tributary of Firth River. Type section designated along south slope of mountain north of Joe Creek, 18.5 km (11.5 mi) N 68 deg W from point where Joe Creek crosses Canadian boundary, 68 deg 59'30"N, 141 deg 26'W, northern part of Table Mountain quad, northeastern AK. Also exposed in mountains along southern edge of Demarcation Point quad and in many sections along north front of Brooks Range. At type consists of (ascending): dusky-yellow limy mudstone and calcareous siltstone (about 200 ft thick), chert and siliceous siltstone (about 90 ft thick), and calcarenite and bioclastic limestone. Total thickness is 372 ft at type. Transgressive onto underlying Wahoo Limestone of Lisburne Group. Conformably underlies Ikiakpaurak Member (new) of Echooka Formation. Age ranges from Wolfcampian (early Sakmarian) to Guadalupian (early Kazanian) based on brachiopod fauna. [Thus age is Early and Late Permian].

Source: GNU records (USGS DDS-6; Menlo GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).