The Plates Forces Pulling Or Pushing I'm In 6th Grade And I Know This
where two plates pull apart from each other at oceanic ridges
A divergent boundary forms when two plates pull apart. As the plates move away from each other, magma rises to fill the gap, creating new crust. This process can result in the formation of mid-ocean ridges.
A rift valley forms when plates pull apart. This results in the Earth's crust stretching and thinning, creating a long, narrow depression with steep walls. Examples include the East African Rift and the Mid-Atlantic Ridge.
A shield volcano forms where plates pull apart. This type of volcano has gentle sloping sides and is characterized by its low viscosity lava flows. Examples of shield volcanoes include those in Hawaii.
As tectonic plates pull apart at spreading boundaries, magma rises from the mantle to fill the gap, creating new oceanic crust. This process forms features like mid-ocean ridges, rift valleys, and volcanic activity along the boundary. Over time, as the plates continue to move apart, the new crust cools and solidifies, adding to the ocean floor.
a valley or a canyon
a rift hope i helped
where two plates pull apart from each other at oceanic ridges
A divergent boundary forms when two plates pull apart. As the plates move away from each other, magma rises to fill the gap, creating new crust. This process can result in the formation of mid-ocean ridges.
A rift valley forms when plates pull apart. This results in the Earth's crust stretching and thinning, creating a long, narrow depression with steep walls. Examples include the East African Rift and the Mid-Atlantic Ridge.
A mid-ocean ridge forms when two sections of oceanic crust move apart from each other. Magma wells up from beneath the Earth's crust to fill the gap, creating new oceanic crust in the process. Over time, this process leads to the formation of underwater mountain chains.
When there is a divergent boundary, regardless if the plates are ocean-ocean or continental-continental, tensional stress pulls on the crust. Rocks have weaker tensional strength than compressive strength, so they are easier to pull apart.
A shield volcano forms where plates pull apart. This type of volcano has gentle sloping sides and is characterized by its low viscosity lava flows. Examples of shield volcanoes include those in Hawaii.
A divergent boundary forms when tectonic plates pull apart. As the plates move away from each other, magma rises up to create new crust, resulting in features like mid-ocean ridges or rift valleys on land.
Stress that acts to pull materials (including rocks of the crust) apart is known as tensile stress.
When the two plates are pulled apart it forms a Constructive Plate Boundary. When it is pulled apart, a big hole is made so material from the mantle fills the void and creates a new crust. It can be seen as a wound for example, a scab begins to repair the wound but any stress cracks it apart, that causes the blood (mantle) to ooze back in again to reform a new scab (crust).Hope I helped :)wrong...it's divergent.
As tectonic plates pull apart at spreading boundaries, magma rises from the mantle to fill the gap, creating new oceanic crust. This process forms features like mid-ocean ridges, rift valleys, and volcanic activity along the boundary. Over time, as the plates continue to move apart, the new crust cools and solidifies, adding to the ocean floor.