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- The Pacific Ocean has a highly varied topography12that includes oceanic ridges, trenches, and seamounts12. The oceanic ridges are underwater mountain ranges that mark the boundaries of tectonic plates. The trenches are deep and narrow depressions that form where one plate subducts under another. The seamounts are isolated volcanic peaks that rise from the ocean floor. Some of them reach the surface and form islands, such as Hawaii1. The ocean floor also has continental slopes and abyssal plains2, which are the sloping and flat regions of the continental margins and the deep ocean basins.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.
The Pacific Ocean has a highly varied topography that consists of oceanic ridges, trenches, and long seamount chains that are formed by hotspot volcanoes under the Earth's surface. An example of these seamounts that are above the ocean's surface are the islands of Hawaii.
www.thoughtco.com/geography-of-the-pacific-ocea…The main features of the Pacific Ocean floor are the continental slopes, which drop from about 200 m to several thousand metres over a distance of a few hundred kilometres; the abyssal plains — exceedingly flat and from 4,000 m to 6,000 m deep; volcanic seamounts and islands; and trenches at subduction zones that are up to 11,000 m deep.
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