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The mountains are one of the numerous climatic factors. They represent natural barriers for the air masses, meaning that they can stop the air masses, modify them, cause precipitation, or dry winds. When the air masses come upon a mountain, they start to build up as they are not able to pass through it. This results in condensation and precipitation on the windward side of the mountain, making the windward side having much more moderate and wetter climate. On the other side, the leeward side gets only dry air masses going down. This makes makes this side of the mountain warmer and dry, often resulting in arid or semi-arid climates.
A convergent-plate boundary to the west of North America caused oceanic crust to be subducted, causing collisions with microcontinents and the partial melting of oceanic crust to create the Sierran volcanic arc.
<h3>Give an explanation of the plate tectonic conditions that led to the formation of the Sevier thrust belt and the Sierran arc. During the Laramide orogeny, what happened?</h3>
A convergent-plate boundary to the west of North America caused oceanic crust to be subducted, which led to collisions with microcontinents and the partial melting of oceanic crust that produced the Sierran volcanic arc. Compression was responsible for the arc's folds and thrust faults. As opposed to earlier orogenies that just established the more superficial faults of the fold-thrust belts behind the arc, faulting associated with the Laramide orogeny was responsible for the creation of the Rocky Mountains. The Sevier-style orogeny may have changed as a result of the subducting slab's shallowing dip.
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