INDUS RIVER

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INDUS RIVER

1. Indus River – Introduction

The Indus River is one of the most important rivers in Asia and among the longest rivers of the Indian subcontinent. It originates near Lake Manasarovar from the Senge Zangbo Glacier in Tibet (China), flows through India (Ladakh) and Pakistan, and finally empties into the Arabian Sea. The river is approximately 3,180 kilometres long. It is closely associated with the ancient Indus Valley Civilization, one of the world's earliest urban civilizations. The Indus is a lifeline for agriculture, drinking water, irrigation, and hydroelectric power, supporting millions of people across its basin.

2. Geographical Facts about the Indus River

The Indus River rises near Mount Kailash and Lake Manasarovar in the Tibetan Plateau. It flows northwest through Ladakh, enters Gilgit-Baltistan in Pakistan, and continues southward across the country before forming a large delta near Karachi and entering the Arabian Sea. The river drains a basin of approximately 1.165 million square kilometres, covering parts of China, India, Pakistan, and Afghanistan. It flows mainly from north-east to south-west. The upper course passes through rugged Himalayan terrain, while the lower course flows through fertile plains that support extensive agricultural activities.

3. Major Tributaries and Cities of the Indus River

The Indus River has several important tributaries, including the Jhelum, Chenab, Ravi, Beas, Sutlej, Shyok, and Zanskar rivers. Together, these rivers form one of South Asia's largest river systems. Important cities along or near the Indus include Leh (India), Gilgit, Skardu, Attock, Sukkur, and Karachi (near the delta) in Pakistan. These cities depend on the river for water supply, irrigation, transportation, and economic activities. The tributaries contribute significant water from the Himalayas, making the Indus River system one of the world's most important snow-fed river networks.

4. Major Features of the Indus River