Pls im desperate and on a timer i will give brainliest answer which increases along faults and leads to rock breaking? damage earthquake focus stress the image shows mountains in alaska. which statements describe these mountains? check all that apply. a syncline is visible. an anticline is visible. these mountains show no evidence of folding. these mountains likely formed from compression. these mountains likely formed from normal faults. the image shows the great rift valley in africa, an example of a rift valley. which statements best describe how the great rift valley in africa formed? check all that apply. the rift valley formed when the crust pulled apart. the rift valley formed at a divergent boundary. the rift valley formed similarly to an island arc. the rift valley formed at a convergent boundary. the rift valley formed when tectonic plates separated. what causes the force that pushes magma from the magma chamber through the pipe and vent of a volcano? gravity water flow expanding gases convergent boundaries

An earthquake is created by tectonic plates becoming united and placing a force on the ground. The tension grows so great that rocks give way by cutting and driving along fault extensions.

Mountain embodiment relates to the geological methods that hold the extension of mountains. Various aerial enduring continental margins various reasonable share the identical mechanism of uplift. where folding is created by horizontal compression operating on a thin to the thick crust development zone .

The Rift Valley was created by powerful subterranean oppression that ripped aside the earth's crust. These powers prompted huge parts of the crust to decline between parallel lapse lines and drive up the molten stone in volcanic explosions.

As they rise, gas particles in the magma arise out of suspension and make bubbles and as the bubbles rise they expand. Eventually, the pressure from these bubbles is greater than the enclosing solid rock and this neighboring rock fissures, letting the magma to get to surface.

velocity and height

rocks and weathering-matching