Gravitational sliding:Plate motion is driven by the higher elevation of plates at ocean ridges. As oceanic lithosphere is formed at spreading ridges from hot mantle material it gradually cools and thickens with age (and thus distance from the ridge).
Gravitational sliding:Plate motion is driven by the higher elevation of plates at ocean ridges. As oceanic lithosphere is formed at spreading ridges from hot mantle material it gradually cools and thickens with age (and thus distance from the ridge).
A tectonic force is the push between the tectonic plates
No, temperature does not affect the force of gravity. Gravity is a fundamental force of nature that is determined by the mass and distance between objects, not by temperature. Temperature may affect the properties of objects or materials, but it does not influence the strength of gravity.
The force that is causing movement at this fault is called tectonic force. These forces are generated by the movement and interaction of the Earth's tectonic plates.
The greater the mass, the stronger the gravity, but the distance does not affect the amount of gravity.
Increasing the mass of a protective container does not affect the force of gravity acting on it. The force of gravity is determined by the mass of the planet or celestial body the container is on and the distance from the center of that body. The mass of an object does not affect the force of gravity acting on it.
No, convection currents in the mantle are the primary driving force behind the movement of tectonic plates. These currents are generated by heat from the Earth's core, causing movement in the mantle that in turn drags and moves the overlying tectonic plates.
The force of Gravity.
Tectonic plates are responsible for the formation of mountains. When two tectonic plates collide, the force can cause the Earth's crust to uplift and fold, resulting in the formation of mountain ranges. This process is known as orogeny.
Mountains are the land form most changed by the force of gravity over time. Gravity causes erosion, landslides, and the shifting of tectonic plates, which all contribute to the constant changes in the shape and height of mountains.
air pressure
Gravity