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Key Facts about Nazca Ridge

31-08-2024

08:26 AM

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1 min read
Key Facts about Nazca Ridge Blog Image

Overview:

A team of oceanographers recently discovered and mapped a new seamount on the Nazca Ridge in international waters, 900 miles off the coast of Chile.

About Nazca Ridge:

  • It is a submarine ridge located in the southeastern Pacific Ocean off the coast of South America.
  • It is approximately 1,100 kilometers (684 miles) long and varies in width.
  • The ridge extends from the Nazca Plate, off the coast of Peru, and runs southwest toward Easter Island, Chile.
  • It was formed by volcanic activity associated with a hotspot in the Earth's mantle.
  • The ridge is composed of abnormally thick basaltic ocean crust.
  • The ridge is tectonically active and is being subducted beneath the South American Plate at the Peru-Chile Trench.

What is a Seamount?

  • A seamount is an underwater mountain with steep sides rising from the seafloor.
  • Most seamounts are remnants of extinct volcanoes. 
  • Typically, they are cone-shaped but often have other prominent features such as craters and linear ridges, and some, called guyots, have large, flat summits
  • There is a broad size distribution for seamounts, but to be classified as a seamount, the feature must have a vertical relief of at least 1,000 meters (3,300 feet) above the surrounding seafloor.
  • Seamounts are found in every world ocean basin.
  • These are formed near mid-ocean ridges, where the earth’s tectonic plates are moving apart, allowing molten rock to rise to the seafloor.
  • Some seamounts have also been found near intraplate hotspots – regions of heavy volcanic activity within a plate – and oceanic island chains with a volcanic and seismic activity called island arcs.

Q1: What is ocean crust?

Oceanic crust, the outermost layer of Earth’s lithosphere that is found under the oceans and formed at spreading centres on oceanic ridges, which occur at divergent plate boundaries. Oceanic crust is about 6 km (4 miles) thick. It is composed of several layers, not including the overlying sediment. The topmost layer, about 500 metres (1,650 feet) thick, includes lavas made of basalt (that is, rock material consisting largely of plagioclase [feldspar] and pyroxene).

Source: Ocean World Exploration: A New Seamount And Previously Unknown Species Discovered