Contours for a gentle slope are spaced equally and far apart, the closer the contour lines the steeper the slope.
When the contour lines are farther apart, this means that the slopes between them are gentle. On the other side, if the contour interval is smaller, the slope will be steep.
At the shoreline
looking at it
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The continental shelf, slope, and rise are all part of the continental margin. The continental shelf is the flat, shallow portion closest to the shore, followed by the continental slope, which descends steeply to the ocean floor. The continental rise is a gentle incline at the base of the continental slope. These features are connected and represent the transition from the continent to the deep ocean basin.
A passive continental rise is a gentle slope between the continental slope and the deep ocean floor. It is formed by sediments that accumulate from the erosional processes on the continental slope. The sediments typically consist of finer grains such as silt and clay.
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.
No, the continental slope is a steeply sloping zone between the continental shelf and the deep ocean floor. It typically has a gradient of approximately 3-6 degrees, making it much steeper than the more gradual continental shelf.
Two different origins for the continental rise are turbidity currents depositing sediments at the base of the continental slope, forming a wedge-shaped accumulation, and sediment transported by rivers accumulating at the continental margin, leading to the gradual build-up of a gentle slope.
The underwater edge of a continent is called the continental shelf. It is a gently sloping underwater landmass that extends from the shoreline to the beginning of the ocean floor.
continental slope
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
Continental slope, Continental Rise, Continental Slope, Seamont, Trench
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
Contours for a gentle slope are spaced equally and far apart, the closer the contour lines the steeper the slope.