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प्रश्न
Describe the relief features of the mountains in north India.
विस्तार में उत्तर
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उत्तर
- Greater Himalayas (Himadri):
- Highest and northernmost range of the Himalayas.
- Always covered with snow, with glaciers and snow-fed rivers.
- Peaks contains the world's highest peaks, including Mount Everest (8,848 meters) and Kanchenjunga (8,586 meters).
- The range forms the main climatic barrier and separates India from the Tibetan Plateau.
- Lesser Himalayas (Himachal):
- Middle range located south of the Greater Himalayas.
- Average elevation ranges from 3,000 to 4,500 meters.
- Famous for hill stations like Shimla, Mussoorie, and Nainital.
- Known for beautiful valleys such as Kullu and Kangra in Himachal Pradesh.
- The Pir Panjal Range and Dhaoladhar Range are part of this system.
- Shiwalik Range (Outer Himalayas):
- Lowest and southernmost range of the Himalayas.
- Made of loose soil and rocks, consisting mainly of alluvial deposits.
- Elevation: Ranges from 900 meters to 1,200 meters above sea level.
- Known for valleys called ‘Duns’, such as the Dehradun, Kothari Dun, and Patli Dun.
- The Shiwaliks are heavily eroded and form the foothills of the higher Himalayan ranges.
- Foothills:
- Between the Shiwalik Range and the plains of India, there are several foothills characterized by rolling terrain and small hills.
- These areas are often fertile and have rich alluvial soils deposited by rivers.
- River Valleys:
- The Himalayas are the source of several major rivers in North India, including the Indus, Ganga, and Brahmaputra.
- These rivers flow through deep valleys, such as the Kashmir Valley and Kathmandu Valley, formed by the uplifting of the mountains and the erosion caused by the rivers.
- Geological Features:
- The Himalayas are young fold mountains, having formed during the Tertiary period, around 50 to 70 million years ago.
- The region is still seismically active, leading to occasional earthquakes and landslides.
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अध्याय 3: Relief - Examination Corner [पृष्ठ ४४]
