When gravitational force and buoyant force are balanced on the lithosphere, the rock is in isostatic equilibrium. This means that the rock is neither sinking nor rising in response to the forces acting on it.
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 buoyant force of the lithosphere floating on the denser underlying mantle and the gravitational force pulling the lithosphere downwards.
Buoyancy force is balanced by the gravitational force acting on an object submerged in a fluid. As an object displaces fluid, it experiences an upward buoyant force equal to the weight of the fluid it displaces, which opposes the gravitational force pulling it downward. When these two forces are equal, the object becomes neutrally buoyant and will float at a constant depth in the fluid.
If the gravitational force is less than the buoyant force, the drag force will act in the opposite direction of the gravitational force.
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.
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 buoyant force of the lithosphere floating on the denser underlying mantle and the gravitational force pulling the lithosphere downwards.
Buoyancy force is balanced by the gravitational force acting on an object submerged in a fluid. As an object displaces fluid, it experiences an upward buoyant force equal to the weight of the fluid it displaces, which opposes the gravitational force pulling it downward. When these two forces are equal, the object becomes neutrally buoyant and will float at a constant depth in the fluid.
If the gravitational force is less than the buoyant force, the drag force will act in the opposite direction of the gravitational force.
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.
The gravitational force and the buoyant force.
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.
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 the force acting on a hot air balloon is balanced, the balloon will remain at a constant altitude. This means that the buoyant force on the balloon is equal to the gravitational force acting on it. As a result, the balloon neither rises nor descends.
by the balance of buoyant and gravitational force
The opposite of buoyant force is gravitational force. Gravitational force acts downwards, pulling objects toward the center of the Earth, while buoyant force acts upwards, pushing objects in a fluid upwards.
Isostasy. It refers to the equilibrium between the weight of Earth's lithosphere (which includes the continents) and the buoyant force exerted by the asthenosphere below, which causes the lithosphere to float.