In a fault-block system, a Graben is the central block of the Earth’s crust that has subsided or dropped down between two parallel faults. This usually occurs due to tensional forces pulling the crust apart. While the uplifted blocks are ...
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Plains are classified as Second-category (Second-order) landforms. First-order landforms are the continents and ocean basins. Second-order landforms are the major features found on them, created by internal tectonic forces, such as mountains, plateaus and plains. Third-order landforms are smaller features ...
The Anatolian Plateau in Turkey is an intermontane plateau located between the Pontic Mountains to the north (along the Black Sea) and the Taurus Mountains to the south (along the Mediterranean). This central highland forms the heart of Turkey, with ...
The Loess Plateau is an Aeolian landform, meaning it was formed by the action of wind. “Loess” is a fine, yellowish-brown silt deposited by wind blowing from the desert regions of Central Asia. Over geological time, this wind-blown dust accumulated ...
The Chota Nagpur Plateau is not an intermontane plateau; it is a continental plateau (or a dissected plateau) located in eastern India. Unlike the Mexican, Tibetan or Bolivian plateaus, which are trapped between mountain ranges, Chota Nagpur is a massive ...