FIG. 62. Zig-zag structure deposited by dune with reversing lee-side spurs and scour pits; Navajo Sandstone (Upper Triassic? and Jurassic) near Escalante, Utah. |
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RECOGNITION: The set of cross-beds in the center of this photograph was deposited by a dune that migrated into the plane of the outcrop. While the dune was migrating, lee-side spurs and scour pits reversed migration direction or asymmetry, thereby creating the zig-zagging sets of cross-beds. Numbers identify the sequence in which specific sets were deposited. Note the alternating dip directions (sets 1 and 3 dip to the left in the outcrop plane; sets 2 and 4 dip to the right). The set of zig-zags is approximately 10 m thick. |
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U.S. Department of the Interior | U.S. Geological Survey | Western Coastal & Marine Geology
URL: http://walrus.wr.usgs.gov/seds/bedforms/photo_pages/pic62.html
Maintained by: Laura Zink Torresan
Modified: 17 October 2006 (lzt)