
Виберіть із наведених ланцюжків причинно-наслідкових зв'язків правильний. Стійкі, вирівняні
ділянки земної кори - давні платформи → рівнини суходолу → найдавніші ділянки земної кори. Рухливі ділянки земної кори → літосферні плити → молоді платформи → гори - найдавніші ділянки земної кори

Ответы на вопрос

Ответ:+ Стійкі, вирівняні ділянки земної кори – давні платформи — рівнини суходолу — найдавніші ділянки земної кори.
Объяснение:



Chain of Causal Relationships in Earth's Crust
The correct chain of causal relationships in the Earth's crust is as follows:
Stable, aligned sections of the Earth's crust - ancient platforms → continental plains → oldest sections of the Earth's crust.
Mobile sections of the Earth's crust → lithospheric plates → young platforms → mountains - oldest sections of the Earth's crust.
This chain of causal relationships describes the geological processes that have shaped the Earth's crust over time. The Earth's crust is composed of several tectonic plates that float on the semi-fluid asthenosphere beneath them. These plates are constantly moving due to the convective currents in the mantle.
The stable, aligned sections of the Earth's crust, known as ancient platforms, are the oldest parts of the crust. Over time, these ancient platforms have undergone erosion and sedimentation, resulting in the formation of continental plains.
On the other hand, the mobile sections of the Earth's crust are characterized by tectonic activity and movement. These mobile sections are divided into lithospheric plates, which are large, rigid pieces of the Earth's crust. The movement of these plates can result in various geological phenomena, such as earthquakes, volcanic activity, and the formation of mountains.
As the lithospheric plates collide, they can create compressional forces that uplift the Earth's crust, leading to the formation of mountains. These mountains are often found in areas where the Earth's crust is relatively young, as the older sections have undergone more extensive erosion and weathering.
In summary, the chain of causal relationships in the Earth's crust starts with stable, aligned sections of the crust (ancient platforms), which give rise to continental plains. The mobile sections of the crust (lithospheric plates) then lead to the formation of young platforms and, ultimately, mountains in the oldest sections of the Earth's crust.


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