Final answer:
The continental rise forms at a passive margin as a result of sediment accumulation from various processes. It is a gentle slope between the continental slope and the abyssal plain.
Step-by-step explanation:
The continental rise forms at a passive margin as a result of sediment accumulation from various processes. At a passive margin, tectonic activity is no longer present, and the sediments are deposited in deeper marine environments. These sediments, including fine particles and carbonates, build up gradually, forming a gentle slope known as the continental rise. The continental rise is typically found between the continental slope and the abyssal plain.