Indian drainage system Flashcards
Drainage Pattern Definition
The pattern formed by river channels and their tributaries as they flow across the landscape, influenced by geology and topography.
Dendritic Drainage Pattern
Resembles the branches of a tree, with tributaries joining the main river at acute angles. Example: Ganga and its tributaries.
Trellis Drainage Pattern
Forms when tributaries flow parallel to each other and join the main river at right angles, common in folded mountains. Example: Narmada and Son rivers.
Radial Drainage Pattern
Rivers flow outward in all directions from a central point, usually from a dome or volcanic cone. Example: Rivers from Amarkantak hills (like Narmada and Son).
Centripetal Drainage Pattern
Rivers flow inward from different directions into a central depression or basin. Example: Rivers draining into Sambhar Lake, Rajasthan.
Rectangular Drainage Pattern
Forms when rivers follow fault lines or fractures in a grid-like pattern, joining at right angles. Example: Streams in the Vindhyan region.
Parallel Drainage Pattern
Rivers flow parallel to each other, typically in areas with steep slopes. Example: Small rivers along the Western Ghats.
Annular Drainage Pattern
Rivers form concentric circles around a central uplifted area, flowing along fractures or weaker rocks. Rare in India but seen in some hilly terrains.
Superimposed Drainage
Rivers cut across geological structures, maintaining their original course even when terrain changes. Example: Chambal River.
Antecedent Drainage
Rivers that existed before the uplift of land and continue to flow by cutting through rising terrain. Example: Indus and Brahmaputra rivers.
Consequent Drainage
Rivers that flow in the direction of the slope or initial uplift of the land. Example: Godavari and Krishna rivers.
Significance of Drainage Patterns
They shape the landscape, influence agriculture, determine water availability, and affect human settlements and infrastructure.
Ancient River: Shiwalik or Indo-Brahma
Geologists believe that during the Miocene period (approximately 5-24 million years ago), a mighty river called the Shiwalik or Indo-Brahma traversed the entire length of the Himalayas, from Assam to Punjab, discharging into the Gulf of Sind near lower Punjab.
Dismemberment into Three Systems
Over time, the Indo-Brahma river was divided into three major drainage systems: (i) The Indus and its tributaries in the western part, (ii) The Ganga and its Himalayan tributaries in the central part, and (iii) The Brahmaputra and its tributaries in the eastern part.
Causes of Dismemberment
The division of the Indo-Brahma river is attributed to geological events during the Pleistocene epoch, including the uplift of the Potwar Plateau (Delhi Ridge), which acted as a water divide between the Indus and Ganga systems, and the down-thrusting of the Malda gap area between the Rajmahal hills and the Meghalaya plateau, diverting the Ganga and Brahmaputra towards the Bay of Bengal.
Antecedent Rivers
Rivers such as the Indus, Satluj, and Brahmaputra are considered antecedent rivers, meaning they existed before the Himalayan uplift and maintained their course by cutting through the rising mountains, forming deep gorges.
Formation of Gorges and Valleys
As the Himalayas uplifted, rivers like the Indus and Brahmaputra carved out deep gorges through erosional activity, a process that occurred simultaneously with the mountain building.
Origin of the Indus River
The Indus River originates from a glacier near Bokhar Chu in the Tibetan region at an altitude of 4,164 meters in the Kailash Mountain range. In Tibet it is also known as “Singhi Khamban” AKA- Lions mouth
Course through India
Flowing west, the Indus enters India in the Ladakh region of Jammu and Kashmir, forming a picturesque gorge in this part.
Course through Pakistan
The Indus flows through Baltistan and Gilgit, emerging from the mountains at Attock, where it receives the Kabul River on its right bank.
Confluence of Panjnad
Near Mithankot in Pakistan, the Indus is joined by the Panjnad, a confluence of five rivers: the Satluj, Beas, Ravi, Chenab, and Jhelum.
Termination Point
The Indus River flows southward and eventually discharges into the Arabian Sea, east of Karachi.
Length and Basin Area
With a total length of 2,900 km, the Indus is one of the longest rivers in the world, covering a basin area of 1,165,000 sq. km, of which about 321,289 sq. km lies in India.
Indus Water Treaty (1960)
According to this treaty between India and Pakistan, India can utilize only 20% of the total water carried by the Indus river system, primarily for irrigation in Punjab, Haryana, and parts of Rajasthan.