river watershed
Because, drainage basins are high elevated
At a transform plate boundary, the motion is horizontal and parallel to the boundary. The plates slide past each other in opposite directions, causing earthquakes due to the friction between the plates. This type of boundary is also known as a strike-slip boundary.
A ridge that directs water flow in opposite directions on either side is called a watershed or a drainage divide. It serves as the boundary between two drainage basins, where precipitation on one side drains into one river or lake, while water on the other side drains into a different body of water. This geographical feature plays a crucial role in hydrology and the management of water resources.
A divergent plate boundary will form between India and Australia when they move in different directions. This boundary will result in the two plates moving away from each other, leading to the formation of new crust as magma rises to the surface.
There are two main types of watersheds: drainage divides and drainage basins. Drainage divides separate different watersheds by defining the boundary between them. Drainage basins collect water and channel it towards a common outlet, such as a river, lake, or ocean.
A sliding boundary is a type of boundary that allows for relative motion between two plates, typically characterized by horizontal movement in opposite directions along the boundary. It often results in shearing or rubbing of rock material along the boundary, causing earthquakes. Deformation and striations on the rocks can be evidence of sliding boundaries.
Convergent: plates move into one another.Divergent: plates move apart.Transform: plates move sideways in relation to each other.
Equilibrant vector is the opposite of resultant vector, they act in opposite directions to balance each other.
When two forces are acting on an object in opposite directions, we combine them by finding the difference between the magnitudes of the two forces. The direction of the resulting force will be in the direction of the larger force.
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Unequal forces acting in opposite directions create a net force that will cause an object to accelerate in the direction of the greater force. The resulting motion depends on the difference between the forces and the mass of the object.
A spreading boundary is a geological term used to describe the boundary between two tectonic plates that are moving away from each other. This separation leads to the formation of new crust through volcanic activity and the upwelling of molten rock from the mantle. One example of a spreading boundary is the Mid-Atlantic Ridge.