The temperature of the continental rise is the temp of your dick
No, active continental margins typically do not have a continental rise. Instead, they often have a steep continental slope that descends into a deep oceanic trench due to tectonic activity. Continental rises are found at passive continental margins where there is minimal tectonic activity.
The accumulation of sediment at the bottom of a continental slope is referred to as continental rise. This phenomenon occurs in oceans throughout the world.
The continental margin consists of the continental shelf, continental slope, and continental rise. One feature that is not part of the continental margin is the abyssal plain, which lies deeper in the ocean and beyond the continental rise. The abyssal plain represents the flat, deep-sea floor that extends across the ocean basins, while the continental margin is specifically associated with the transition from land to ocean.
A continental rise forms where the continental slope levels off, and sediment accumulates due to gravity transporting sediments downslope from the slope above. This is a gentle accumulation of sediments deposited by turbidity currents, rivers, and other geological processes at the base of the slope.
If the shape of the meniscus is concave up then the cohesive forces are weaker than the adhesive forces. If the shape of the menicus is concave down then the adhesive forces are weaker than the cohesive forces. So capillary rise is where adhesive forces are stronger.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
continental margin
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
continental rise
The oceanic crust begins at the continental rise
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the transition zone between the continent and the deep ocean basin.
continental rise
downslope from the continental shelf
The continental shelf, continental slope, and continental rise together form the continental margin. The continental margin is the submerged edge of a continent that consists of these three distinct but connected features.
The temperature of the continental rise is the temp of your dick
The Continental rise is often hundreds of kiometres. But in the pacific ocean it has a greater number.