Continental Margin

continental margin, the submarine edge of the continental crust distinguished by relatively light and isostatically high-floating material in comparison with the adjacent oceanic crust. It is the name for the collective area that encompasses the continental shelf, continental slope, and continental rise. The characteristics of the various continental margins are shaped by a number of factors. Chief among these are tectonics, fluctuations of sea level, the size of the rivers that empty onto a margin as determined by the amount of sediment they carry, and the energy conditions or strength of the ocean waves and currents along the margin.