Yes. Mid Ocean Ridges create new oceanic crust.
it makes mid-oceanic ridges
Mid-Ocean ridges.
B. Larger. Mid-ocean ridges are underwater mountain ranges where tectonic plates are spreading apart, allowing magma to rise and create new oceanic crust. This process contributes to the growth of oceans.
the cause is erosion and long something
Ridges under the ocean are primarily created by tectonic processes, specifically the movement of tectonic plates at mid-ocean ridges. As these plates diverge, magma from the mantle rises to fill the gap, solidifying to form new oceanic crust. This process not only creates ridges but also contributes to the formation of underwater volcanic activity and seismic events. Additionally, the upwelling of hot magma can create elevated features on the ocean floor, resulting in the characteristic topography of mid-ocean ridges.
Divergent boundaries create landforms such as rift valleys and mid-ocean ridges. Rift valleys form on continents when land is pulled apart, while mid-ocean ridges develop along the ocean floor as new crust is created.
Ocean ridges are generally located along the boundaries of tectonic plates, primarily in the middle of ocean basins. They form where plates are diverging, allowing magma to rise from the mantle and create new oceanic crust. This process can be observed in major oceanic ridges such as the Mid-Atlantic Ridge and the East Pacific Rise. These ridges are characterized by elevated topography and volcanic activity.
Mid-Ocean Ridges
The Mid-Ocean ridges were first discovered in the 1950's
No, divergent plate boundaries can occur both on the ocean floor and on land. When they occur on the ocean floor, they create mid-ocean ridges, while on land they can create rift valleys.
Sea floor spreading creates new oceanic crust at mid-ocean ridges. Magma rises to the surface, cools, and solidifies to form new crust as tectonic plates move apart. This process contributes to the continuous expansion of the ocean floor.
Compared to ocean crust near deep-sea trenches, crust near ocean ridges is generally younger, thinner, and hotter. Ocean ridges are sites of active seafloor spreading where magma rises to create new crust, while deep-sea trenches are associated with subduction, where older, denser crust is pulled back into the mantle. As a result, the crust at ocean ridges is also less dense and more buoyant than the crust found near trenches.