As the sheets of oceanic crust move away from the mid-ocean ridge, the rock is cooled and thus becomes heavier. After about 200 million years, the cooled Lithospheric plate has become heavier than the Asthenosphere that it rides over, and it sinks, thereby producing a subduction zone.
No
at mid ocean ridges
It is true that mid-ocean ridges are underwater mountain ranges. These ridges are where the lithosphere is moving apart and new oceanic crust is being formed.
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
there both oceans and They both have mid-ocean ridges.
No
go to google and type mid ocean ridge, and there will be pictures of oceans with ridges!
yes
at mid ocean ridges
Moraine is the term used to describe ridges of rock debris left behind by a moving glacier. These ridges can vary in size and shape depending on the glacier's motion and the material it carries. They are a key feature in understanding the past movements of glaciers and their impact on the landscape.
mid-ocean ridges tey are under water.
Ridges of rock debris that form in front of a glacier are called terminal moraines at the point that the glacier stops moving ahead.
Ridges and Rises are uplifts in oceanic crust caused by volcanic eruption in oceans, the difference between a ridge and a rise is of rift valleys, ridges have long valleys and rises do not have any valleys
It is true that mid-ocean ridges are underwater mountain ranges. These ridges are where the lithosphere is moving apart and new oceanic crust is being formed.
It is true that mid-ocean ridges are underwater mountain ranges. These ridges are where the lithosphere is moving apart and new oceanic crust is being formed.
It is true that mid-ocean ridges are underwater mountain ranges. These ridges are where the lithosphere is moving apart and new oceanic crust is being formed.