Question

Схема образования_______________и________________складок.Области складчатости формируются там,где слои земной коры___________,а движения литосферных плит направлены___________друг другу. Схема начала образования складок и________

Answer 1

Схема образования выпуклых и вогнутых складок.Области складчатости формируются там, где слои земной коры смяты в складки, а движение литосферных плит направлено навстречу друг к другу.

Answer 2

Formation of Fold Mountains and Fold Structures

The formation of fold mountains and fold structures is a result of tectonic forces acting on the Earth's crust. These forces lead to the development of folded rock layers and mountain ranges. The areas of fold formation are typically where the Earth's crust is subjected to compression, and the movements of lithospheric plates are directed towards each other.

Formation of Fold Mountains and Fold Structures: The process of fold formation begins with the convergence of tectonic plates, leading to compression and the development of folded rock layers. This process is associated with the formation of fold mountains, which are characterized by extensive folding and faulting of the Earth's crust.

Areas of Fold Formation: Areas of fold formation are primarily located where the Earth's crust experiences compression due to tectonic forces. This compression leads to the folding of rock layers and the formation of fold structures. These areas are often associated with convergent plate boundaries, where tectonic plates move towards each other.

Direction of Plate Movements: The movements of lithospheric plates at convergent boundaries are directed towards each other. This convergence results in the compression of the Earth's crust, leading to the formation of fold mountains and fold structures.

Summary: In summary, the formation of fold mountains and fold structures is a result of compression in the Earth's crust, typically occurring at convergent plate boundaries where tectonic plates move towards each other. This process leads to the development of folded rock layers and the creation of prominent mountain ranges.

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