Ocean Floor
The ocean floor is the bottom of the ocean, which varies in depth from shallow waters such as coral reefs and continental shelves to deep ocean trenches and abyssal plains. The ocean floor is composed of different types of sediments, rocks, and minerals, and is home to a diverse range of marine life. The topography of the ocean floor is shaped by various geological processes such as tectonic activity, volcanic eruptions, and erosion. The study of the ocean floor is important for understanding oceanic processes, marine ecosystems, and for identifying potential resources such as oil and gas deposits, minerals, and deep-sea organisms.
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