Question

При воздействии каких сил (внутренних или внешних) вершины Кавказских гор и Алтая приобрели остроконечную форму?

Answer 1

Внешних таких как передвижение воздушных масс

Answer 2

Forces that Shaped the Sharp Peaks of the Caucasus Mountains and Altai Mountains

The sharp, cone-like shape of the peaks in the Caucasus Mountains and Altai Mountains can be attributed to a combination of internal and external forces. These forces have acted over millions of years to shape the landscape we see today.

Internal Forces: Internal forces refer to the geological processes that occur within the Earth's crust. These forces include tectonic activity, volcanic eruptions, and the movement of the Earth's plates. In the case of the Caucasus Mountains and Altai Mountains, the following internal forces have played a role in shaping their sharp peaks:

1. Tectonic Activity: The Caucasus Mountains and Altai Mountains are located in regions where tectonic plates collide. The collision of these plates has resulted in the uplift of the land, leading to the formation of mountain ranges. The intense pressure and compression associated with tectonic activity have contributed to the formation of sharp peaks in these mountain ranges.

2. Volcanic Activity: Volcanic eruptions have also played a role in shaping the sharp peaks of these mountains. Volcanic activity can result in the deposition of volcanic materials, such as lava and ash, which can build up over time and contribute to the formation of steep slopes and sharp peaks.

External Forces: External forces refer to the processes that occur on the Earth's surface, such as erosion and weathering. These forces have also played a significant role in shaping the sharp peaks of the Caucasus Mountains and Altai Mountains. The following external forces have contributed to the formation of their distinctive cone-like shape:

1. Glacial Erosion: Glaciers have been instrumental in shaping the landscape of these mountain ranges. As glaciers move, they erode the underlying rock, carving out valleys and creating sharp peaks. The grinding action of the ice and the weight of the glacier can result in the formation of steep, pointed peaks.

2. Weathering and Mass Wasting: Weathering refers to the breakdown of rocks into smaller particles, while mass wasting refers to the movement of these particles down slopes. Both processes can contribute to the formation of sharp peaks by wearing away the surrounding rock and leaving behind more resistant materials that form the peaks.

In conclusion, the sharp, cone-like shape of the peaks in the Caucasus Mountains and Altai Mountains is the result of a combination of internal forces, such as tectonic activity and volcanic eruptions, as well as external forces, including glacial erosion, weathering, and mass wasting. These forces have acted over millions of years to shape the landscape we see today.