Continental crust over a divergent boundary can typically be found at mid-ocean ridges, where tectonic plates are pulling apart. In some cases, such as the East African Rift, divergent boundaries can also occur on land, leading to the formation of rift valleys. These regions are characterized by volcanic activity and geological features associated with the thinning and stretching of the continental crust.
When a hotspot rises and cracks the surface, it is typically associated with a divergent boundary. At divergent boundaries, tectonic plates move apart, allowing magma from the mantle to rise up and create new crust.
A normal fault is typically found on a divergent boundary. This type of fault occurs as the Earth's crust is being pulled apart, causing one side to move downward relative to the other.
No, folded mountain ranges are typically found in areas of continental collision, where tectonic plates are pushed together and the crust is folded and uplifted. Mid-ocean ridges are divergent plate boundaries, where plates are moving apart and new oceanic crust is being created, so folded mountain ranges would not be expected there.
You would find a mid-ocean ridge at an oceanic-oceanic plate divergent boundary. This ridge is formed by the spreading apart of the two plates, allowing magma to rise and create new oceanic crust.
You would find divergent plate boundaries in the Atlantic Ocean, specifically along the Mid-Atlantic Ridge. This is where tectonic plates are moving apart, leading to the formation of new oceanic crust.
This would be called a Spreading center, or a divergent plate boundary.
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The East African Rift Valley
At a divergent plate boundary, where new crust is created by infilling magma, creating igneous rock.
A divergent plate boundary would have less silica content compared to a convergent plate boundary. Divergent boundaries involve the separation of tectonic plates, with new oceanic crust forming from magma that is relatively low in silica content. In contrast, convergent boundaries involve the collision of tectonic plates, resulting in the melting of crust with higher silica content, leading to more explosive volcanic activity.
When a hotspot rises and cracks the surface, it is typically associated with a divergent boundary. At divergent boundaries, tectonic plates move apart, allowing magma from the mantle to rise up and create new crust.
A normal fault is typically found on a divergent boundary. This type of fault occurs as the Earth's crust is being pulled apart, causing one side to move downward relative to the other.
When oceanic crust is pushed under continental crust in a subduction zone, a deep trench is formed at the boundary between the two plates. The oceanic crust then descends into the mantle, creating a convergent plate boundary. This process can lead to the formation of volcanic arcs on the overriding continental plate.
it would be more likely to occur at convergent ocean-continental boundary beacuse the rocks are composed with a higher silica and has much thicker continental crust.
You would need to find a continental rift. The best example of an active continental rift is the East African Rift.
You would find a mid-ocean ridge at an oceanic-oceanic plate divergent boundary. This ridge is formed by the spreading apart of the two plates, allowing magma to rise and create new oceanic crust.
No, folded mountain ranges are typically found in areas of continental collision, where tectonic plates are pushed together and the crust is folded and uplifted. Mid-ocean ridges are divergent plate boundaries, where plates are moving apart and new oceanic crust is being created, so folded mountain ranges would not be expected there.