TRUE
as downward line
It has a negative (downward) slope.
Angle od decent is the certain angle that an objecy uses, such as a ramp, to move another object, such as a ball, downward.
neg x-axis is from the origin to the left.neg y-axis is from the origin down.There's no such thing as a negative line.On the common Cartesian (x - y) graph, 'y' decreases and goes negative as you move downward, 'x' decreases and becomes negative as you move to the left,and a line with negative slope tilts downward as it proceeds from left to right.
entrapment
Yes, the continental slope descends steeply from the continental shelf into the deep ocean floor. It marks the boundary between the continental crust and the oceanic crust.
Yes, the continental slope drops downward to the edge of the continent at which point it plummets down for the depth of the continental plate. It depends upon whom you speak with, but a nation's boundary is generally considered 200 miles beyond that.
The continental slope is the steep transition between the continental shelf and the deep ocean floor, marking a distinct boundary in underwater topography. This area typically descends at an angle of 2 to 5 degrees, leading to the abyssal plain. It serves as a critical ecological zone where nutrients from the shelf can flow into deeper waters, supporting diverse marine life. Additionally, the slope is important for geological studies and resource exploration, including oil and gas deposits.
A syncline is a downward fold in rock layers where the youngest rocks are in the center and the oldest rocks are towards the edges. It forms a U shape, with the limbs of the fold dipping towards the center.
The part of a continent that dips gently downward and is underwater is called the continental shelf. When a continent drops steeply in to the ocean it is called a continental slope.
continental slope
CONTINENTAL SLOPE
continental shelf
A convergent plate boundary is caused by a downward convection current in the mantle. At these boundaries, tectonic plates move towards each other, resulting in subduction zones or collision zones, where one plate is forced beneath the other.
The continental shelf
The answer is: B. Continental slope.
The force pushing upward on the continental crust is isostatic rebound, caused by the buoyancy of the less dense continental crust floating on the denser mantle. The downward force is from the weight of the overlying rock and sediments, as well as tectonic forces like subduction or compression.