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Mariana islands, island arc, a series of volcanic and uplifted coral formations in the western pacific ocean, about 1,500 miles (2,400 km) east of the philippines. Discover geology, marine life, and exploration history. Dive into the mariana trench, earth's deepest point, where extreme conditions harbor unique marine life and profound geological features.
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The mariana trench is the deepest part of the world's oceans, located in the western pacific ocean Explore the mariana trench, earth's deepest ocean frontier reaching 11,000m below sea level The weight of the ocean above it creates pressure around 15,750 pounds per square inch (more than 1,000 times what we experience on land) and the alien world is devoid of light.
The pacific plate is subducted beneath the mariana plate, creating the mariana trench, and (further on) the arc of the mariana islands, as water trapped in the plate is released and explodes upward to form island volcanoes and earthquakes.
The mariana trench is a prime example of a subduction zone, where the pacific plate is being subducted beneath the smaller mariana plate As the pacific plate is denser and older, it keeps sinking into the earth’s mantle under the mariana plate. The mariana islands (also the marianas Up to the early 20th century sometimes called islas de los ladrones meaning islands of thieves) are a group of islands made up by the summits of 15 volcanic mountains in the western pacific ocean.
Roman feminine form of marianus After the classical era it was sometimes interpreted as a combination of maria and ana In portuguese it is further used as a form of mariamne The mariana islands are the southern part of a submerged mountain range that extends 1,565 miles (2,519 km) from guam to near japan
Geographically, the marianas are part of a larger region called micronesia, situated between 13° and 21°n latitude and 144° and 146°e longitude.
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