Where are the mountains on Earth that best reflect vertical zonality?

Kilimanjaro. There are two reasons for this, latitude and altitude. The influencing factor of the vertical zone of mountains is heat.

If the latitude is low, there will be a natural zone of low latitude, and if the altitude is high, there will be a natural zone of high latitude. And Kilimanjaro is the most satisfying of this condition, the most complete, from low latitudes to high latitudes. Some people will think that it is Mount Everest, but because of the higher latitude, the natural zone at the lower latitudes is missing.

Yunnan-Guizhou Plateau. Because it is a molten limestone mountain.

Summary. East African Plateau: Vertical Zone.

The altitude of this area is more than 3,000 meters, and due to the high terrain, the temperature and precipitation conditions here have changed, and the climate is warm, and the tropical rainforest climate cannot be formed. In summer, under the influence of the warm and humid southeast monsoon from the Indian Ocean that passes over the warm current, there is more precipitation, forming a wet season. In winter, the order is accepted.

1. Dry monsoon control, less precipitation, and vigorous ground evaporation, forming a dry season.

What are the plateaus formed by the vertical movement of the earth's crust.

Loess plateau. Can you ask us a little more about the causes of the East African plateau?

East African Plateau: Vertical Zone.

East African Plateau: Vertical Zone. The altitude of this area is more than 3,000 meters, and due to the high terrain, the temperature and precipitation conditions here have changed, and the climate is warm, and the tropical rainforest climate cannot be formed.

In summer, under the influence of the warm and humid southeast monsoon from the Indian Ocean that passes over the warm current, there is more precipitation, forming a wet season. In winter, the order is accepted.

1. Dry monsoon control, less precipitation, and vigorous ground evaporation, forming a dry season.

Plateau genesis is not climatic cause.

This is where the land mass separates, i.e. in eastern Africa, which is exactly in the zone of strong upwelling of mantle material. Under the action of upwelling, the East African crust is uplifted to form plateaus.

Mountains [shān mài].

Topography. A mountain range is a mountain that extends in a certain direction and consists of several mountains and valleys. Mainly due to the action of internal forces in the movement of the earth's crust, there are obvious folds, which are different from mountains, while mountains are under the action of a certain force, and the fold phenomenon is not obvious.

The composition of the mountain range includes the main mountain (main trunk), the major branch, the small branch, and the residual vein. The residual vein is relatively small, and it is separated from the main trunk or large branch by a long low warm zone.

Monolithic Mountains and Scattered Mountains: The former is on an overall plateau, for example, the Tianshan Mountains are an integral highland; The latter has a certain integrity, but it is not on a monolithic plateau, for example, the north and south of Wugong Mountain in the middle of the Luoxiao Mountains are a long low warm zone.

The level of the mountains varies according to their size. For example, Wugong Mountain in the Luoxiao Mountains itself is a relatively large mountain range, including some small mountains and many mountains. The Tianshan Mountain Range, which stretches for thousands of miles, is a group of large mountain ranges, large mountain range suits, medium-sized mountain ranges, and medium-sized mountain ranges on the super large mountain range set line.

Because the sunlight from the remnants of the panicle is abundant in the low-latitude areas, the temperature difference from the foot of the mountain to the top of the mountain is relatively large, and there are many plants suitable for various temperatures, so there are many types of plants.

In the high latitudes, the temperature difference from the base of the mountain to the top of the mountain is not too large, and the temperature at the bottom of the mountain is also relatively low, and there are many fewer plants growing at low temperatures than at normal temperatures, so there are not many plant species from the bottom of the mountain to the top of the mountain.

As for the most typical of it, it is because there is a different plant not far away, and you can see many different plants at a glance. And in the high latitudes, there is always a forest of one and another forest, which is a large area.

I'm easy enough to understand, give some points.