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April 01, 1989
Presence of rounded boulders and large cobbles at base of White River Group (Oligocene) strata in Southwest North Dakota and Northwest South Dakota
Eric N. Clausen
Eric N. Clausen
Minot State Univ., Div. Sci., Minot, ND, United States
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Rocky Mountain Geology (1989) 27 (1): 1–6.
Article history
first online:
03 Mar 2017
Citation
Eric N. Clausen; Presence of rounded boulders and large cobbles at base of White River Group (Oligocene) strata in Southwest North Dakota and Northwest South Dakota. Rocky Mountain Geology 1989;; 27 (1): 1–6. doi:
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Index Terms/Descriptors
- boulders
- Brule Formation
- Cenozoic
- Chadron Formation
- clastic rocks
- clastic sediments
- cobbles
- conglomerate
- Dunn County North Dakota
- Harding County South Dakota
- lower Oligocene
- North Dakota
- Oligocene
- Paleogene
- sedimentary rocks
- sediments
- Slope County North Dakota
- South Dakota
- Stark County North Dakota
- stratigraphy
- Tertiary
- United States
- White River Group
- Chalky Buttes
- Killdeer Mountains
- Little Badlands
- northwestern South Dakota
- Rainy Buttes
- Reva Gap
- Short Pine Hills
- Slim Buttes
- southwestern North Dakota
- White Butte
Latitude & Longitude
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