The Continental Rise is a gently sloping area found at the base of the continental slope, where the ocean floor begins to level out. It is formed by the accumulation of sediments that have washed down from the land and the continental shelf. This region plays a crucial role in the ocean's ecosystem, providing habitats for various marine life. The rise is typically made up of thick layers of sediment, including sand, mud, and other materials. These sediments can come from rivers, glaciers, and even volcanic activity. The Continental Rise is an important part of the ocean's structure, connecting the land to the deep sea and influencing ocean currents and marine biodiversity.