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In mountainous course, the Himalayan rivers form gorges.Explanation:
Mountainous Course of Himalayan Rivers:
The Himalayan region is characterized by its high peaks, deep valleys, and rugged terrain. The rivers in this region have a steep gradient due to the presence of mountains. As these rivers flow through the mountains, they undergo various erosional and depositional processes, resulting in the formation of distinct landforms.
Gorges:
Gorges are narrow, steep-sided valleys with high vertical walls that are formed by the erosive action of rivers. In the case of Himalayan rivers, the fast-flowing water cuts through the hard rock layers of the mountains, gradually deepening and widening the valley. Over time, these erosional processes create a deep and narrow gorge. The steep slopes of the gorges are often covered with dense vegetation, adding to the scenic beauty of these landscapes.
Factors contributing to Gorge formation:
Several factors contribute to the formation of gorges in mountainous regions:
- Upliftment: The tectonic upliftment of the Himalayas results in the creation of high mountain ranges. The rivers flowing through these mountains encounter steep slopes, leading to the erosion and formation of gorges.
- Erosion: The fast-flowing water of the rivers carries sediments, rocks, and debris. This material acts as a powerful erosive agent, gradually wearing away the rocks and deepening the valley.
- Differential erosion: The Himalayan mountains consist of different types of rocks with varying resistance to erosion. Softer rocks are eroded more quickly, while harder rocks are eroded at a slower pace. This differential erosion leads to the formation of gorges with distinct rock formations and vertical cliffs.
- Tectonic activity: The Himalayas are a seismically active region, experiencing frequent earthquakes and faulting. These tectonic activities can further contribute to the formation and modification of gorges by altering the landscape and river courses.
Conclusion:
In summary, the mountainous course of Himalayan rivers, characterized by steep slopes and rugged terrain, leads to the formation of gorges. The erosive action of fast-flowing water, upliftment of the Himalayas, differential erosion, and tectonic activity all play a role in shaping these spectacular landforms. Gorges not only serve as natural marvels but also have ecological significance, providing habitats for various plants and animals.