File:Theodore Roosevelt National Park Slump Formation.jpg

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Theodore_Roosevelt_National_Park_Slump_Formation.jpg ‎(640 × 480 pixels, file size: 324 KB, MIME type: image/jpeg)

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English: A slumping tilted strata rock formation — within Theodore Roosevelt National Park, in North Dakota.
  • The tilted mounds in slump formations formed when the streams that cut into the cliffs over-steepened them. Heavy Moisture led to land slides of blocks of overhanging earth. Thus the slumps retained their original layering sequence.
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Author M. Readey

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current18:43, 18 November 2011Thumbnail for version as of 18:43, 18 November 2011640 × 480 (324 KB)Circa24 (talk | contribs)

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