Question

Срочно тектонична будова антрактыды​

Answer 1

Рельєф і тектонічна будова материка. Велика східна частина Антарктиди представляє собою давню Антарктичну платформу з докембрійським фундаментом

Answer 2

Tectonic Structure of the Carboniferous Period (Antarcticy)

The tectonic structure of the Carboniferous period, also known as the Antarcitcyd, was characterized by significant geological events and movements that shaped the Earth's surface during that time.

Formation of Supercontinent: During the Carboniferous period, the supercontinent Pangaea began to form as a result of the collision of several smaller landmasses. This tectonic event had a profound impact on the Earth's geography and climate.

Mountain Building: The collision of tectonic plates during the Carboniferous period led to the formation of major mountain ranges, such as the Appalachian Mountains in North America and the Ural Mountains in Russia. These mountain-building processes were instrumental in shaping the topography of the Earth during this time.

Coal Formation: The tectonic activity during the Carboniferous period also played a crucial role in the formation of extensive coal deposits. The compression of plant matter in swampy environments, combined with tectonic forces, led to the creation of coal seams that are still exploited today.

Glaciation: Tectonic movements during the Carboniferous period also contributed to significant glaciation events, particularly in the southern hemisphere. These glacial periods had a substantial impact on global sea levels and the distribution of land and water.

Summary: In summary, the tectonic structure of the Carboniferous period, or Antarcticyd, was characterized by the formation of Pangaea, mountain-building processes, the creation of coal deposits, and significant glaciation events. These tectonic activities had a lasting impact on the Earth's geological and geographical features.