A tectonic force is the push between the tectonic plates
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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.
It is a force that could be contributing or complementing mantle convectional currents in the movements of lithospheric or tectonic plates. This force is generated when there is friction between convectional currents and the lithospheric or tectonic plate that lies above.
The force that pulls tectonic plates toward each other is known as "slab pull." This occurs when a dense oceanic plate descends into the mantle at a subduction zone, generating a gravitational force that pulls the rest of the plate along with it.
The force that pulls apart the crust is called tensional or extensional tectonic stress, which occurs at divergent plate boundaries where tectonic plates move away from each other. This pulling force can lead to the formation of rift valleys and mid-ocean ridges.
Mount Semeru, located in Indonesia, is primarily affected by the Indo-Australian plate subducting beneath the Eurasian plate. This subduction zone causes the tectonic force that leads to the volcanic activity and uplift of Mount Semeru.
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Friction
Our Tectonic plates shifting and moving around.
The force that squeezes together the crust is called compression. This force is usually caused by tectonic plate movements, which can lead to the folding and faulting of rock layers.
Tectonic plate movements or plate shifting.
The force that works against isostatic adjustment is typically referred to as tectonic forces. These forces include compression, extension, and shear created by the movement of tectonic plates. These forces can cause the crust to deform and adjust, disrupting the isostatic equilibrium.