Final answer:
Subduction stops at oceanic-oceanic convergent boundary, forming mountain ranges like the Andes.
Explanation:
Subduction stops occurring at an oceanic-oceanic convergent boundary, resulting in a mountain range. This process involves one oceanic plate subducting beneath another oceanic plate, leading to the formation of volcanic arcs and trenches.
One example of this is the formation of the Andes Mountains where the Nazca plate subducts beneath the South American plate, creating a chain of coastal volcanic mountains.
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