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
The continental rise is located at the base of the continental slope, where the incline lessens and sediment from the continent accumulates. It marks the transition between the continental margin and the deep ocean basin.
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.
continental slope
The continental shelf and the continental slope together make up the continental margin. The continental shelf is a gently sloping extension of the continent underwater, while the continental slope is a steeper drop-off that leads to the ocean floor.
The area you are referring to is known as the continental rise. It is located at the base of the continental slope and consists of a thick accumulation of sediments that have been transported down from the continent. The continental rise marks the transition between the continental margin and the deep ocean basin.
The portion of the continental margin that serves as a boundary between the oceanic crust and the continental crust is called the continental shelf. This is the shallowest part of the margin, located between the shoreline and the 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.