Plate collisions form different types of mountains, including folded and fault-block mountains. Dome and volcanic mountains have similarities in their upward movement but differ in magma involvement.
Convergent Boundaries: occur when two plates collide, leading to mountain formation. Types include continent-continent convergence, continent-ocean convergence, and ocean-ocean convergence. Folded Mountains: form when two continental plates collide, causing the Earth's crust to buckle and fold, creating mountain ranges like the Alps.
Fault-Block Mountains: form when tensional forces lead to blocks of crust being uplifted, creating mountain ranges with steep slopes and flat tops. Dome vs. Volcanic Mountains: Dome mountains form from uplifted, arched rock layers, while volcanic mountains form from volcanic eruptions. Both involve upward movement, but dome mountains do not involve magma.
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