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Trans-Alaska Pipeline in front of Albian-Cenomanian strata of the Torok and Nanushuk Formations (contact at base of lowest prominent sandstone bench), exposed on Marmot syncline about 100 miles south of Prudhoe Bay. This section represents a generally progradational succession from shelf or prodelta at the base to upper shoreface or delta front at the top.
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Trans-Alaska Pipeline in front of Albian-Cenomanian strata of the Torok and Nanushuk Formations (contact at base of lowest prominent sandstone bench), exposed on Marmot syncline about 100 miles south of Prudhoe Bay. This section represents a generally progradational succession from shelf or prodelta at the base to upper shoreface or delta front at the top.