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Short-run macroeconomic equilibrium occurs when the quantity of real GDP demanded
Seafloor Spreading
The process by which new oceanic crust is formed at mid-ocean ridges and moves away from the ridge, contributing to continental drift.
Subduction
When tectonic plates converge, the movement of one plate beneath another into the mantle is referred to as subduction.
Continental Margins
The zones of the ocean floor that separate the thin oceanic crust from thick continental crust, including the continental shelf, slope, and rise.
Seafloor Spreading
The formation of new oceanic crust at mid-ocean ridges and its gradual movement away from the ridge.
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