rift valley
Answer 2
Continents are formed when continental plates pull apart.
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∙ 9y agoWhen continental plates pull apart, they form rift valleys. This process is known as rifting and it can ultimately lead to the formation of new ocean basins if the plates continue to separate.
A rift valley forms at the place where two continental plates pull apart. This process is known as continental rifting, and it can eventually lead to the formation of a new ocean basin if the rifting process continues and is accompanied by seafloor spreading.
A rift valley is created when two continental plates pull apart. This process forms a large trench-like depression on land, often accompanied by volcanic activity and earthquakes. An example of this is the East African Rift Valley.
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.
When Earth's crust pulls apart, a geological feature known as a rift valley can form. This process is called rifting and can lead to the creation of new ocean basins where magma rises to fill the gap created by the separation of the crustal plates.
A Rift Valley can form when tectonic plates pull apart, creating a linear depression or valley. The crust stretches and thins, causing the land to sink and creating a low-lying valley with steep sides. Examples include the East African Rift Valley and the Great Rift Valley in Africa.
rift valley Answer 2 Continents are formed when continental plates pull apart.
It forms a rift valley.
Tectonic plates do pull apart in the middle of the ocean. These divergent plates form what is known as the Mid-Atlantic ridge.
Divergent plate boundaries form once two plates begin to pull apart from each other.
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
A rift valley forms at the place where two continental plates pull apart. This process is known as continental rifting, and it can eventually lead to the formation of a new ocean basin if the rifting process continues and is accompanied by seafloor spreading.
It forms at a plate boundary. It deepens as the plates pull apart.
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.
This will form a series of tensile features. Initially, normal faulting will occur, then horst and graben structures will form and ultimately a rift valley will develop.
A rift valley is created when two continental plates pull apart. This process forms a large trench-like depression on land, often accompanied by volcanic activity and earthquakes. An example of this is the East African Rift Valley.
When continental plates pull apart at a divergent boundary on land, it can lead to the formation of rift valleys. Magma rises to the surface creating new crust, which can eventually separate the landmass into two distinct plates. Over time, this process can create new ocean basins if the divergence continues.
divergent plates