DRAINAGE SYSTEMS NOTES - #CLASS9#GEOGRAPHY

 DRAINAGE SYSTEMS NOTES - #CLASS9#GEOGRAPHY

·        Drainage: Describes the river system of an area.

·        Drainage Basin: The area drained by a single river system.

·        Water Divide: An elevated area (like a mountain or upland) that separates two drainage basins. Example: Ambala separates the Indus and Ganga river systems.

·        The world's largest drainage basin is the Amazon river.

DRAINAGE SYSTEMS IN INDIA

Indian rivers are divided into two main groups based on relief features:

1.     Himalayan Rivers

2.     Peninsular Rivers

1. Himalayan Rivers

·        Characteristics:

o   Most are

perennial (have water throughout the year).

o   Receive water from rain and melted snow.

o   Long courses from source to sea.

o   Perform intensive erosional activity in upper courses, carrying huge loads of silt and sand.

o   Form meanders, ox-bow lakes, and deltas in middle and lower courses.

o   Cut through mountains making gorges.

·        Major Himalayan Rivers:

o   Indus River System:

§  Origin: Tibet, near Lake Mansarowar.

§  Enters India in Ladakh, forming a picturesque gorge.

§  Tributaries in Kashmir: Zaskar, Nubra, Shyok, Hunza.

§  Tributaries joining near Mithankot (Pakistan): Satluj, Beas, Ravi, Chenab, Jhelum.

§  Flows southwards to the Arabian Sea.

§  Total length: 2900 km (one of the longest rivers).

§  About one-third of the basin is in India (Ladakh, J&K, Himachal Pradesh, Punjab).

§  Indus Water Treaty (1960): India can use 20% of the water for irrigation.

o   Ganga River System:

§  Headwaters: 'Bhagirathi' (from Gangotri Glacier) and Alaknanda.

§  Confluence: They meet at Devaprayag in Uttarakhand to form the Ganga.

§  Emerges onto plains at Haridwar.

§  Himalayan Tributaries: Yamuna (rises from Yamunotri Glacier, meets Ganga at Allahabad), Ghaghara, Gandak, Kosi (rise in Nepal Himalaya, cause floods but enrich soil).

§  Peninsular Tributaries: Chambal, Betwa, Son (from semi-arid areas, shorter courses, less water).

§  Flows eastwards, bifurcates at Farakka into Bhagirathi-Hooghly (distributary) and mainstream.

§  Mainstream enters Bangladesh, joined by Brahmaputra, then known as Meghna.

§  Forms the Sundarban Delta (world's largest and fastest-growing, home to Royal Bengal tiger).

§  Length: Over 2500 km.

§  Gentle slope in plains leads to large meanders.

o   Brahmaputra River System:

§  Origin: Tibet, east of Mansarowar lake.

§  Slightly longer than the Indus; most of its course is outside India.

§  Known as Tsang Po in Tibet.

§  Enters India at Namcha Barwa (Arunachal Pradesh) through a gorge, called Dihang.

§  Joined by Dibang, Lohit, and other tributaries to form Brahmaputra in Assam.

§  In Tibet, carries smaller volume of water and less silt (cold, dry area).

§  In India (high rainfall region), carries large volume of water and considerable silt, forming braided channels and riverine islands.

§  Causes widespread floods in Assam and Bangladesh due to rising riverbed from silt deposits.

2. Peninsular Rivers

·        Main Water Divide: Western Ghats.

·        Characteristics:

o   Mostly

seasonal (flow dependent on rainfall).

o   Reduced water flow during dry seasons.

o   Shorter and shallower courses compared to Himalayan rivers.

o   Drainage basins comparatively smaller.

·        East Flowing Rivers (Drain into Bay of Bengal):

o   Most originate in the Western Ghats.

o   Make deltas at their mouths.

o   Mahanadi Basin: Rises in highlands of Chhattisgarh, flows through Odisha to Bay of Bengal. Length: ~860 km. Basin shared by Maharashtra, Chhattisgarh, Jharkhand, Odisha.

o   Godavari Basin: Largest Peninsular river. Rises from Western Ghats (Nasik). Length: ~1500 km, drains into Bay of Bengal. Known as Dakshin Ganga. Basin covers parts of Maharashtra, Madhya Pradesh, Odisha, Andhra Pradesh.

o   Krishna Basin: Rises near Mahabaleshwar, flows ~1400 km to Bay of Bengal. Tributaries: Tungabhadra, Koyana, Ghatprabha, Musi, Bhima. Basin shared by Maharashtra, Karnataka, Andhra Pradesh.

o   Kaveri Basin: Rises in Brahmagiri range (Western Ghats), reaches Bay of Bengal in Tamil Nadu. Length: ~760 km. Tributaries: Amravati, Bhavani, Hemavati, Kabini. Basin drains parts of Karnataka, Kerala, Tamil Nadu. Forms Shivasamudram Falls (second biggest waterfall in India).

o   Other smaller east-flowing rivers: Damoder, Brahmani, Baitarni, Subarnrekha.

·        West Flowing Rivers (Drain into Arabian Sea):

o   The Narmada and Tapi are the only long rivers flowing west.

o   Make estuaries instead of deltas.

o   Narmada Basin: Rises in Amarkantak hills (MP). Flows west in a rift valley due to faulting. Forms picturesque locations like 'Marble rocks' and 'Dhuadhar falls'. Tributaries are short and join at right angles. Basin covers parts of Madhya Pradesh and Gujarat.

o   Tapi Basin: Rises in Satpura ranges (Betul, MP). Flows in a rift valley parallel to Narmada, but shorter. Basin covers parts of Madhya Pradesh, Gujarat, and Maharashtra.

o   Other short coastal west-flowing rivers: Sabarmati, Mahi, Bharathpuzha, Periyar.

LAKES

·        Vary in size and characteristics; most are permanent, some seasonal.

·        Formation: Glacial action, wind, river action, human activities.

·        Types:

o   Ox-bow lakes: Formed by meandering rivers cutting off.

o   Lagoons: Formed by spits and bars in coastal areas (e.g., Chilika, Pulicat, Kolleru).

o   Saltwater lakes: In regions of inland drainage, sometimes seasonal (e.g., Sambhar Lake in Rajasthan, used for salt production).

o   Freshwater lakes: Mostly in Himalayan region, often of glacial origin (formed by glaciers, filled with snowmelt).

o   Tectonic Lakes: Wular Lake (J&K) is the result of tectonic activity and is the largest freshwater lake in India.

o   Other important freshwater lakes: Dal Lake, Bhimtal, Nainital, Loktak, Barapani.

o   Artificial Lakes: Formed by damming rivers for hydel power (e.g., Guru Gobind Sagar/Bhakra Nangal Project).

·        Importance of Lakes:

o   Regulate river flow (prevent floods, maintain even flow).

o   Generate hydel power.

o   Moderate climate.

o   Maintain aquatic ecosystem.

o   Enhance natural beauty.

o   Develop tourism and provide recreation.

ROLE OF RIVERS IN THE ECONOMY

·        Basic Natural Resource: Essential for various human activities.

·        Historical Significance: Riverbanks have attracted settlers and led to the development of big cities since ancient times.

·        Agriculture: Crucial for irrigation, especially in agrarian economies like India.

·        Navigation: Used for transportation.

·        Hydro-power Generation: A significant source of energy.

RIVER POLLUTION

·        Increasing domestic, municipal, industrial, and agricultural demand reduces river volume.

·        Heavy load of untreated sewage and industrial effluents degrade water quality and reduce the river's self-cleansing capacity.

·        Increasing urbanization and industrialization lead to rising pollution levels.

·        Government initiatives like the Ganga Action Plan (GAP, 1985) and National River Conservation Plan (NRCP, 1995) aim to improve water quality through pollution abatement.

 

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