Facts about Ocean Floor Topography
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Challenger Deep in the Mariana Trench plunges approximately 10,935 meters below sea level, making it the deepest known point on Earth's ocean floor.
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Seamounts, which are underwater volcanoes rising from the ocean floor without reaching the surface, number in the tens of thousands across the world's ocean basins.
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Hydrothermal vents, first discovered in 1977 near the Galápagos Rift, are a dramatic feature of ocean floor topography that support unique chemosynthetic ecosystems.
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Sonar mapping technology, particularly multibeam echosounders, has allowed scientists to chart ocean floor topography in far greater detail than the surface of Mars or the Moon.
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Abyssal plains, which cover much of the deep ocean floor, are among the flattest and smoothest surfaces on Earth, formed by sediment burial of underlying topography.
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The ocean floor topography includes mid-ocean ridges, deep-sea trenches, abyssal plains, and seamounts, making it as varied as any continental landscape.