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The continental margin off northeastern Taiwan consists of five major physiographic units which are the East China Sea continental shelf, the East China Sea continental slope, the Southern Okinawa Trough, the Ilan continental shelf and the Ilan Ridge. This physiographic framework is provisional and may be revised if better physiographic names are proposed. The East China Sea continental shelf is relatively wide with a smooth surface marked locally by low-relief features resulting from sea-level fluctuation during the late Pleistocene and by volcanic activities of the back-arc rifting. The East China Sea continental slope varies laterally in slope gradient and topography. The continental slope is marked is marked by a variety of slumping of sliding scars, erosional gullies, and debris flow deposits of turbidites. The submarine canyons are another prominent topographic feature occurring on the slope. The submarine canyons indent the continental shelf and modify the linear shelf-slope transtition region in to an irregular shape. The western end of the Southern Okinawa Trough has curvelinear bathymetric contours at the maximum depth of about 2,000m. The trough is mainly confined by the continental slope to the north and by sloper off the Ryukyu volcanic islands.

Physiographic Characteristics of the continental Margin, Northeast Taiwan