What Kilimanjaro was called after it ceased geological activity

The Great Rift Valley still has crustal movement to this day, and Kilimanjaro is the result of more recent volcanic activity. It began about 750,000 years ago and originally consisted of three large craters: Sheila, Kibo and Mavents.

Then the Cone of Hilla collapsed and disappeared, followed by Mavinz. However, Kibo has remained alive and there was a massive eruption about 360,000 years ago, which released black lava that overshadowed the Hira crater and formed the Kilimanjaro saddle on the site of Mavenz Volcano.

Kilimanjaro was formed by a combination of tectonic and volcanic activity.

Tectonic movement refers to the formation of plate movements in the Great Rift Valley.

Volcanic activity is that Kilimanjaro is a volcano and is affected by volcanic activity.

There are two main reasons for the rapid demise of Mount Zama: first, natural factors, such as crustal movement and climate change; The second is the anthropogenic factors of Bipei, such as human exploitation that destroys the ecological balance of nature, as well as the activity of volcanic ash and volcanic ash lava.

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Analysis: The place where the plate splits can occur in two situations:

First, if the plate splits in the ocean, then a ridge should be formed. Because the oceanic crust on the ocean floor is thinner than the continental crust on the land, magma gushes out and cools to form ridges.

For example, in the middle of the Atlantic Ocean, due to the American plate, the Eurasian plate and the African plate form a mid-ocean ridge (ridge).

Second, if the plate is on the continent, then a rift valley should be formed. Because the continental crust is thicker than the oceanic crust, there is very little volcanic magma gushing. For example, the Great Rift Valley, which stretches from the Zambezi estuary in southern Africa to the Red Sea and the Mediterranean Sea in the Wulian chain, of course, there are a small number of volcanoes, such as Mount Kilimanjaro!

The trench is formed by the subduction of the large plate to the oceanic side of the continental plate, so it is the boundary of squeezing extinction.

Summary: The earth was torn apart, but magma burst out in the cracks, and when it cooled, it was Qili bending and fighting Ma Za to make trouble for Sun Luoshan

Kilimanjaro stared at Zheng Bore.

The formation is associated with the activities of the Great Rift Valley. More than 10 million years ago, the earth's crust was fractured here, and there was strong volcanic activity along the fault line, Mount Kilimanjaro.

It is made from a large amount of lava accumulation. The peaks above about 5,000 meters are covered with permanent glaciers, which can reach up to 80 meters thick, forming the "Snow Peak Wonder" near the equator. Now due to global climate change.

or increased volcanic activity, the Kilimanjaro mountain glaciers are retreating. According to research, at this rate, Kilimanjaro is likely to have completely melted within a century or two.

The formation of Mount Kilimanjaro is closely related to geological processes. Mount Kilimanjaro is a volcanic mountain that was formed about 1 million years ago during the Quaternary period. It was formed by a series of volcanic eruptions and magma eruptions.

Kilimanjaro is made up of three separate mountains, namely Kibo, Mawenzi and Shira. Among them, the Snow Mountain is the main peak of Kilimanjaro and the highest peak on the African continent.

The formation of Kilimanjaro went through a process of multiple eruptions and magma gushing. During the eruption, magma emerges from deep underground and accumulates to form a mountain. Over time, volcanic activity waned and the mountain began to cool and solidify.

The formation of glaciers also had an impact on the morphology of Kilimanjaro. Due to the high altitude and cold climatic conditions, the summit of Kilimanjaro is covered with glaciers and snow-capped peaks. These glaciers shape the shape of the peaks during the cycle of melting and freezing at the summit.

Overall, the formation of Mount Kilimanjaro was formed by the interweaving of volcanic activity, magma eruptions, and the action of glaciers, resulting in the magnificent mountain landscape that it is today.