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Why can a supply curve be used to measure producer surplus
Continental Crust
The thick, buoyant part of the earth's crust that forms the continents and continental shelves, distinguished from the denser oceanic crust.
Continental Collision
A geological process where two continental plates collide, leading to the formation of mountains and other geological structures.
Subduction Zones
areas at convergent plate boundaries where one tectonic plate moves under another, leading to geological activity.
Plate Boundaries
Plate boundaries are the edges where two or more of Earth's tectonic plates meet, categorized into three types: divergent, convergent, and transform, each characterized by specific geological activities and processes.
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