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Fig. 14.6 Bedforms possibly produced or modifi ed by internal
tidal currents. ( a ) Unidirectional linguoid ripples from the Scotia
Sea southeast of Tierra del Fuego in 4,010 m water depth
(Modifi ed from Heezen and Hollister 1964 ) . ( b ) Current linea-
tions from a fl at-fl oored trough near Reunion Island, Indian
Ocean in 4,909 m water depth (Modifi ed from Heezen and
Hollister 1964 ) . ( c ) Scours around pebbles and cobbles in
1,304 m water depth, Suruga Bay, Japan (Modifi ed from Okada
and Ohta 1993 )
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