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.
A line with slope of zero is horizontal. A line with no slope is vertical because slope is undefined on a vertical line.
positive slope negative slope undefined slope zero slope
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.
Yes. The continental rise is the deepest portion of the continental margin (shelf and slope). The underwater continental shelf extends from the shore to the continental slope, the lower end of the slope being the continental rise, at which sediments can accumulate. Beyond this is the "abyssal plain" which is oceanic crust.
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 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.
I'm text-based and cannot display images. However, you can easily find pictures of the continental slope by doing an image search on the internet. The continental slope is the steep slope that leads from the continental shelf to the deep ocean floor.
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.