GEOLOGY

Detailed explanation-1: -This bubbled-up magma is cooled by frigid seawater to form igneous rock. This rock (basalt) becomes a new part of Earth’s crust. Mid-Ocean Ridges Seafloor spreading occurs along mid-ocean ridges-large mountain ranges rising from the ocean floor.

Detailed explanation-2: -Mid-ocean ridges form at divergent plate boundaries, where seafloor spreading leads to the production of new ocean crust. This new crust is formed due to igneous intrusions and extrusions as magma either cools beneath the Earth’s surface or erupts as lava above the Earth’s surface.

Detailed explanation-3: -Magmatic and tectonic processes at mid-ocean ridges form oceanic crust and accommodate relative plate motions. Oceanic lithosphere forms and becomes denser as the plate moves away from the mid-ocean ridge and cools.

Detailed explanation-4: -Oceanic crust is continuously being created at mid-ocean ridges. As continental plates diverge at these ridges, magma rises into the upper mantle and crust. As the continental plates move away from the ridge, the newly formed rocks cool and start to erode with sediment gradually building up on top of them.

Detailed explanation-5: -The divergent boundaries are the areas where plates are moving apart from one another. Where plates move apart, new crustal material is formed from molten magma from below the Earth’s surface. Because of this, the youngest sea floor can be found along divergent boundaries, such as the Mid-Atlantic Ocean Ridge.