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  3. Unconformity between the Triassic Dinwoody Formation and basal conglomerate of the Lower Cretaceous Kootenai Formation. Beaverhead County, Montana. nd.

Unconformity between the Triassic Dinwoody Formation and basal conglomerate of the Lower Cretaceous Kootenai Formation. Beaverhead County, Montana. nd.

Summary

Album caption: Unconformity between the Triassic Dinwoody Formation and basal conglomerate of the Lower Cretaceous Kootenai Formation. Location is north of Trapper Creek Road just west of confluence of Sucker Creek, 20 m above road level. Hammer is on unconformity, and plane of hammer is parallel to contact. Angular discordance is about 15 degrees; pebbles of Kootenai conglomerate fill local depressions of the unconformable surface developed in the Dinwoody. Published as figure 13.

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Data Owner :
U.S. Geological Survey
Photographer :
Zen, E-an

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zea00038.jpg thumbnail 635.91 KB image/jpeg
zea00038.tif 9.54 MB image/geotiff

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Available in the U.S. Geological Survey Denver Library Photographic Collection, Zen, E-An Collection.

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