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Chapter 2.Intro Bouma Sequence Classic Bouma Sequence
Plate T-1 Slope By California San Francisco is in the black area near the top. Notice how, in some places, the continental slope appears to bulge out at its base. This occurs as the Pacific Plate, which underlies the area, slides past the North American Plate.
(Copyright 1997 Smithsonian Magazine)
Plate T-2 deep-Sea Worm Deep-sea vestimentiferan tubes photographed near hydrocarbon seeps on the continental slope of the northern Gulf of Mexico.
(from http://aeolus.tamu.edu/Info/hist3.html)
Plate T-3 Basin Evolution Schematic summary of evolution of a basin influenced by turbidite
sedimentatiion.

(USG: kai.er.usgs.gov/surveys/area3/lcs/aapg97/index.html)
Plate T-4 Mile High Cliff MILE-HIGH CLIFF marks the edge of the continental slope west of Florida (C). This undersea
 precipice, known as the Florida Escarpment, stands more than four times as high as the Empire State

 Building. Whereas the tilt of the continental slope elsewhere is typically just a few degrees, the face of the escarpment is, on average, slanted at 35 degrees. In many places the walls of the escarpment are near vertical. The seafloor here is made up of the countless skeletons of marine organisms that have cemented together. The gradual accumulation of this material once formed a gently dipping ramp. But some force, perhaps great sweeping currents, eroded the base of the slope.

(Scientific American: http://www.sciam.com/0697issue/0697pratsonbox2c.html)
Plate T-5 Atchafalaya High altitude (62,000 feet) NASA ER-2 near-infrared photograph of the Atchafalaya and Wax Lake deltas and offshore flows of turbid waters, driven by northerly winds.
(The Coastal Studies Institute)

The Clastic Slope Project
Last Revised on June 30, 2006