Tibetan Plateau: An Intermontane Plateau
The question asks to identify the best classification for the Tibetan Plateau based on its geographical features.
Understanding Intermontane Plateaus
- An Intermontane Plateau is a large, raised area of land characterized by its location between mountain ranges.
- These plateaus are often formed by tectonic uplift and are surrounded by significant mountain systems.
Classifying the Tibetan Plateau
- The Tibetan Plateau is situated between the towering Himalayan mountain range to the south and the Kunlun Mountains to the north.
- This geographical positioning perfectly matches the definition of an Intermontane Plateau.
- Therefore, the Tibetan Plateau is the best example of an Intermontane Plateau.
Evaluating Other Options
- Erosional Plateau: Formed by erosion wearing down a high area; the Tibetan Plateau's formation is primarily tectonic.
- Volcanic Plateau: Formed by extensive lava flows; this is not the primary characteristic of the Tibetan Plateau.
- Doomed Plateau: This is not a standard geological or geographical classification for plateaus.
Based on its location nestled between major mountain ranges, the Tibetan Plateau is correctly identified as an Intermontane Plateau.
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Important Questions from Geomorphology
Which one of the following is not an igneous rock?
Which of the following statements is/are correct?
1. Hypocenter is the point on the surface of the Earth, nearest to the focus.
2. Velocity of earthquake waves is higher in denser materials.
3. P waves move faster and are the first to arrive at the surface of the Earth.
Select the correct answer using the code given below:
Which one of the following is the lowermost/innermost intrusive igneous rock?
The formation of ‘tors’ on small rocky hills is associated with which among the following?
Which one of the following statements about metamorphic rocks is not correct?
