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it creates energy
Bubbling in a molten rock creates voids which are called vesicles or vugs.
molten rock bubbles up through the ridge to form new land
At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.
because the molten rock cools in the water and forms a oceanic crust
because the molten rock cools in the water and forms a oceanic crust
At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.
The Mid-Atlantic Ridge (MAR) is a mid-ocean ridge, a divergent tectonic plate boundary located along the floor of the Atlantic Ocean, and part of thelongest mountain range in the world. It separates the Eurasian Plate and North American Plate in the North Atlantic, and the African Plate from the South American Plate in the South Atlantic. The Ridge extends from a junction with the Gakkel Ridge (Mid-Arctic Ridge) northeast of Greenland southward to theBouvet Triple Junction in the South Atlantic. Although the Mid-Atlantic Ridge is mostly an underwater feature, portions of it have enough elevation to extend above sea level. The section of the ridge which includes the island of Iceland is also known as the Reykjanes Ridge. The average spreading rate for the ridge is about 2.5 cm per year.[1]en.wikipedia.org/wiki/Mid-Atlantic_Ridge
As a result of tectonic plates that are moving from each other, the divergent boundaries form rifts, clift valleys or volcanic islands. My gf when we were talking on [dream marriage] also mentioned that those volcanic islands occur when plates move apart to produce gaps which molten lava rises to fill.
In plate tectonics, divergent boundaries occur when plates pull apart. On land, divergent boundaries form rifts or valleys. More commonly, divergent boundaries in the ocean occur and cause mid-oceanic ridges. Divergent boundaries can also form volcanoes when the plates separate enough to allow molten lava to seep out, harden, and eventually form islands.
it creates energy
Bubbling in a molten rock creates voids which are called vesicles or vugs.
The seafloor spreading definition is the geologic process that occurs at the boundary between 2 plates where molten material within the earth pushes its way up, causing the plates to move away from each other. At these divergent boundaries molten material cools and hardens, creating new oceanic crust or seafloor
Mid Ocean Ridges (MOR's). Convection in the asthenosphere causes the plates to pull apart, and new molten earth from the asthenosphere fills the gaps. It occurs deep in the center of the oceans at several places.
Because, the molten material that moves into the fissures and cracks between diverging plates is no thicker than the existing plates. The plate will then probably be destroyed at the other end, due to a convergent boundary :)
In plate tectonics, a Divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other. These areas can form on the end of continents but eventually form ocean basins. Divergent boundaries within continents initially produce rifts which produce rift valleys. Therefore, most active divergent plate boundaries are between oceanic platesand are often called mid-oceanic ridges. Divergent boundaries also form volcanic islands which occur when the plates move apart to produce gaps which molten lava rises to fill. Thus creating a shield volcano which would eventually build up to become a volcanic island.
molten rock bubbles up through the ridge to form new land