Is East African Rift is an example of mid ocean ridge?

If the process continues long enough and the continental crust is effectively separated, the continental rift graben turns into a normal mid-oceanic ridge. … The most prominent example of a continental rift is the East-African Rift Valley and its continuations into the Red Sea and the Gulf of Aden.

What is an example of a rift valley?

Rift valleys are found both on the continents and on the floor of ocean basins. … Other notable examples include the Baikal Rift Valley (Russia) and the Rhine Rift Valley (Germany).

Why Rift Valley has steep sides?

c) Rift valleys have steep sides because they are formed when the earth crust is divided, they are not like those valley which are formed by soil erosion.

How Rift Valley is formed?

A rift valley is a lowland region formed by the interaction of Earth’s tectonic plates. … A rift valley is a lowland region that forms where Earth’s tectonic plates move apart, or rift. Rift valleys are found both on land and at the bottom of the ocean, where they are created by the process of seafloor spreading.

Why did the East African Rift Valley form?

Twenty-five million years ago, as plate tectonics began to pull apart eastern Africa, the landscape that would eventually be home to the first humans began to take shape. … The East African Rift Valley, as the region is known, formed where the Somalian and Nubian plates are pulling away from the Arabian Plate.

What will happen if a Rift Valley continues to pull apart?

If these two rift zones continue they will break apart the crustal plates they are located on and will create new plates. Sea water will flood the rift valleys and they will eventually become seas like the Red Sea.

Which location is on a major rift valley?

The most well-known rift valley on Earth is probably the so-called “Great Rift Valley System” which stretches from the Middle East in the north to Mozambique in the south. The area is geologically active, and features volcanoes, hot springs, geysers, and frequent earthquakes.

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