Sediment-laden Flow of Mooreville Chalk Within the Interior of Wetumpka Marine Target Impact Structure, Alabama: Evidence for a Shallow Water Resurge

Details Sediment-laden Flow of Mooreville Chalk Within the Interior of Wetumpka Marine Target Impact Structure, Alabama: Evidence for a Shallow Water Resurge Sediment-laden Flow of Mooreville Chalk Within the Interior of Wetumpka Marine Target Impact Structure, Alabama: Evidence for a Shallow Water Resurge

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1430o&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1430

Physics

1

Scientific paper

A mudflow deposit with sporadic shocked mineral grains indicates that
the impact occurred in very shallow water. This makes Wetumpka a
uniquely well preserved example of impacts in near-shore environment.

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