Continental shelf.
The slope will be negative.The slope will be negative.The slope will be negative.The slope will be negative.
positive slope negative slope zero slope undefined
The slope of the perpendicular is the negative reciprocal of the slope of a line. In this case, - (1 / -1) = 1.The slope of the perpendicular is the negative reciprocal of the slope of a line. In this case, - (1 / -1) = 1.The slope of the perpendicular is the negative reciprocal of the slope of a line. In this case, - (1 / -1) = 1.The slope of the perpendicular is the negative reciprocal of the slope of a line. In this case, - (1 / -1) = 1.
positive slope negative slope undefined slope zero slope
A line with slope of zero is horizontal. A line with no slope is vertical because slope is undefined on a vertical line.
it dives into a continental slope
it dives into a continental slope
between an abyssal plain and continental slope.
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.
There are not many plants that live in the continental slope. One of the few plants that live here is algae.
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.
They are both part of the larger structure called the continental margin where a continental plate meets an oceanic plate. The lower (deeper) end of the continental slope is called the continental rise.
continental slope
The continental shelf is basically an extension of a continent into an ocean. It is underwater during interglacial periods (such as today) but dry during glacial periods. The continental slope is the sloping area between the continental shelf and the continental rise (where the continental plate meets the oceanic plate). The continental shelf and the continental slope together are called the continental margin. The continental rise is located at the bottom of the continental slope and is formed by the accumulation of sediment from the continent. Past the continental rise lies the abyssal plain which is the flat ocean floor.
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
Here is a pic of the continental slope.
Continental slope, Continental Rise, Continental Slope, Seamont, Trench