Isostasy is a state of gravitational equilibrium where the weight of the Earth's crust is balanced by the buoyancy of the mantle below. This equilibrium is achieved when the crust floats on the denser mantle and remains in equilibrium at a certain level.
When a system is in isostasy, downward gravity and upward buoyancy are balanced.
The gravitational force pulling the crust down and the buoyant force pushing the crust up are balanced in isostasy. This equilibrium allows the Earth's crust to float at a certain level within the asthenosphere.
When a system is in isostasy, downward gravity and upward buoyancy are balanced.
In isostasy, the force of gravity pulling down on the denser materials of the Earth's lithosphere is balanced by the buoyant force pushing up on the less dense asthenosphere below. These two forces reach equilibrium, allowing the lithosphere to "float" at a level where it is in gravitational balance.
When a system is in isostasy, gravitational force pulling down on the higher density material of the crust is balanced by buoyancy force pushing up on the lower density material of the mantle, resulting in equilibrium. This balance allows the Earth's crust to float on the denser material beneath it.
When a system is in isostasy, downward gravity and upward buoyancy are balanced.
The gravitational force pulling the crust down and the buoyant force pushing the crust up are balanced in isostasy. This equilibrium allows the Earth's crust to float at a certain level within the asthenosphere.
When a system is in isostasy, downward gravity and upward buoyancy are balanced.
In isostasy, the force of gravity pulling down on the denser materials of the Earth's lithosphere is balanced by the buoyant force pushing up on the less dense asthenosphere below. These two forces reach equilibrium, allowing the lithosphere to "float" at a level where it is in gravitational balance.
Isostasy is the balance between the weight of the Earth's lithosphere pushing down and the buoyant force of the underlying asthenosphere pushing up. This balance helps to maintain the overall stability of the Earth's crust.
When a system is in isostasy, gravitational force pulling down on the higher density material of the crust is balanced by buoyancy force pushing up on the lower density material of the mantle, resulting in equilibrium. This balance allows the Earth's crust to float on the denser material beneath it.
Isostasy involves the balance between the downward force of gravity acting on the lithosphere and the buoyant force exerted by the asthenosphere below. This balance determines the level of the Earth's crust in response to variations in crustal thickness and density.
You say that the two forces are in equilibrium.
What two forces? If two forces go in opposite directions, and have the same magnitude, they will be balanced. Otherwise they wont'.
If the forces are balanced, then by definition the sum of the forces is zero.
Isostasy is the balance between the buoyant force of the mantle pushing up on the lithosphere and the gravitational force pulling the lithosphere downward. This balance helps maintain the equilibrium of the Earth's crust.
Yes. Two forces that are equal in magnitude but opposite in direction would be balanced.