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Ocean ridges and trenches are related in a few ways. One of the ways is being created from the movement of tectonic plates on the mantle when they diverge and converge. When tectonic platesdiverge they "pull apart" and create trenches. When they converge they "push together" and create ridges, subduction happens here. The tectonic plates move on the mantle of magna from convection currents creating these different boundaries.
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Such type of condition that describes the twisting of the ankle is called an inversion. This condition is not included by the muscle that is responsible for the movement or motion of the hip. There are many muscles that are involved in the movement of the hip such as gluteal muscle, adductor muscle and some other. The longus, brevis muscles are present in the ankle and play an important role in the movement of the ankle.
