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The explanation for the law of demand begins with
Continental Rifting
The pulling apart of a continent, forming a low, fault-bounded trough (continental rift); may lead to a divergent plate boundary that leads to seafloor spreading and splitting apart a continent.
Continental Shelves
Submerged landforms at the edges of continents, extending from the coastline to a sharp drop-off into the deeper ocean floor.
Shallow Seawater
Areas of the ocean that are not deep, often found near coastlines, characterized by relatively low depths.
Sea Mounts
Undersea mountains formed by volcanic activity, rising from the ocean floor but not reaching the surface.
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