WebThe Gakkel Ridge (formerly known as the Nansen Cordillera and Arctic Mid-Ocean Ridge) [1] is a mid-oceanic ridge, a divergent tectonic plate boundary between the North American Plate and the Eurasian Plate. [2] It is located in the Eurasian Basin of the Arctic Ocean, between Greenland and Siberia, and has a length of about 1,800 kilometers ... WebThe mid-ocean ridge is formed where two tectonic plates meet under the ocean. This divergent boundary creates mountains, valleys like the famous rift valley, volcanoes, and …
Oceanic ridge Description, Examples, & Facts Britannica
Web10 de nov. de 2024 · It formed and evolves as a result of spreading in Earth’s lithosphere—the crust and upper mantle—at the divergent boundaries between tectonic … Web• When scientists measured the age of seafloor rocks, they found that younger rocks are closer to the mid-ocean ridges, and older rocks are found closer to trenches. These two pieces of evidence support the idea that the seafloor spreading is valid by showing that the seafloor is not all the same age and is constantly being created at mid ocean ridges … rcs thonon
MODULE 5 SCIENCE PDF Plate Tectonics Continent - Scribd
WebThe East Pacific Rise is a mid-ocean rise (termed an oceanic rise and not a mid-ocean ridge due to its higher rate of spreading that results in less elevation increase and more regular terrain), a divergent tectonic plate … Web28 de ago. de 2024 · A mid-ocean ridge (MOR) is a seafloor mountain system formed by plate tectonics. It typically has a depth of about 2,600 meters (8,500 ft) and rises about 2,000 meters (6,600 ft) above the deepest portion of an ocean basin. This feature is where seafloor spreading takes place along a divergent plate boundary. WebHow mid-oceanic ridges are formed? A mid-ocean ridge or mid-oceanic ridge is an underwater mountain range, formed by plate tectonics. This uplifting of the ocean floor occurs when convection currents rise in the mantle beneath the oceanic crust and create magma where two tectonic plates meet at a divergent boundary. rcs thermostat models