Geology 416M: Sedimentary Rocks Fall 2007
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Course Goals The goals of this course are to learn to identify sedimentary rocks and minerals, and to interpret the processes and environments of their formation. The principles of sedimentology will be examined through lectures and laboratory and field exercises. This course is required for degrees in Geological Sciences and in Petroleum Engineering. Class News
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![]() The Tongue of the Ocean, Bahamas Reef Bank. Andros Island and its west-facing tidal flat environments on platform to west of the ‘Tongue’. At bottom edge (south end) of the tongue are underwater sand dunes that feed sand into the bottom of the tongue. Here at the south end it is about 4,000 feet deep. At the north end where it opens into the Atlantic Ocean it is about 7,000 feet deep. These modern carbonate-forming environments are analogs to the environments of formation of some ancient limestones. NASA Space Shuttle photo, from ESI Outreach Lecture Series CD-ROM v. 2. ![]() The lee face of an eolian dune in Death Valley (California), showing examples of large grain flows, small grain flows, oblique wind ripples (near crest of dune), and vertebrate trace fossils (footprints along left side of photo). Pencil (15 cm) for scale. |
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