<P> The continental margin , between the continental shelf and the abyssal plain , comprises a steep continental slope followed by the flatter continental rise . Sediment from the continent above cascades down the slope and accumulates as a pile of sediment at the base of the slope , called the continental rise . Extending as far as 500 km ( 310 mi ) from the slope , it consists of thick sediments deposited by turbidity currents from the shelf and slope . The continental rise 's gradient is intermediate between the slope and the shelf , on the order of 0.5 -- 1 ° . </P>
<P> The continental margin , between the continental shelf and the abyssal plain , comprises a steep continental slope followed by the flatter continental rise . Sediment from the continent above cascades down the slope and accumulates as a pile of sediment at the base of the slope , called the continental rise . Extending as far as 500 km ( 310 mi ) from the slope , it consists of thick sediments deposited by turbidity currents from the shelf and slope . The continental rise 's gradient is intermediate between the slope and the shelf , on the order of 0.5 -- 1 ° . </P>
what geographical feature of the ocean floor is between the shoreline and the continental slope
what geographical feature of the ocean floor is between the shoreline and the continental slope
continental rise
continental rise