Underwater mountian ranges/ underwater volcanoes
An ocean ridge is most likely to be located at the boundary where two tectonic plates are moving apart, such as the Mid-Atlantic Ridge. This is where new oceanic crust is formed as magma rises to the surface and solidifies, creating a ridge-like structure along the seafloor.
The ocean ridge is most likely to be located along the boundary of tectonic plates, such as the Mid-Atlantic Ridge. This is where new oceanic crust is formed as plates move apart, causing magma to rise and solidify.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust. A classic example is the Mid-Atlantic Ridge where the Eurasian and African Plates are moving away from the North and South American Plates.
No, most of the volcanoes along the mid-ocean ridge do not rise above the ocean's surface. These submarine volcanoes are typically under the water and form part of the continuous volcanic activity that occurs along the ocean ridges. Only a few volcanoes along the mid-ocean ridge, such as Iceland, rise above the ocean's surface.
Oceanic ridge
A mid-ocean ridge is not an underwater volcano. It is a long mountain range on the ocean floor formed by plate tectonics. Underwater volcanoes, also known as seamounts, are mountains that form from volcanic activity on the ocean floor.
The Mid-Atlantic Ridge is neither Continental rock or indeed the oldest rock on the planet. The rock in the ridge is commonly the youngest, or of the youngest, on the planet, as it was formed most recently, and is oceanic, not continental, crustal rock.
i think it happen in mid-ocean ridge.
There are several mid-ocean ridges around the world, with the most well-known being the Mid-Atlantic Ridge, East Pacific Rise, and the Indian Ocean Ridge. These ridges are underwater mountain ranges where tectonic plates are moving apart, creating new ocean crust.
Mid-ocean ridges are formed from the uplift of newly formed oceanic crust by rising magma. As the ridge is slowly pushed away from the source of the heat by the addition of newer crust, it sinks and is no longer part of the ridge, being replaced by new ridge material. This process means that the rock comprising the ridges is among the most recent in geologic age. divergent boundaries
IN the open ocean.
in the ocean