Which drainage pattern is formed by the Central Karbi Anglong Plateau? [#2140]

The Central Karbi Anglong Plateau is characterized by a radial drainage pattern. In this type of pattern, streams flow outward in all directions, like the spokes of a wheel, from a central high point (the plateau). This is a typical pattern for a relatively isolated upland area.

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The Central Karbi Anglong Plateau is characterized by a radial drainage pattern. In this type of pattern, streams flow outward in all directions, like the spokes of a wheel, from a central high point (the plateau). This is a typical pattern for a relatively isolated upland area.

During the winter months, the Brahmaputra River in Assam exhibits a braided drainage pattern.

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During the winter months, the Brahmaputra River in Assam exhibits a braided drainage pattern.

The Vindhya Range separates the Indo-Gangetic Plains of Northern India from the Deccan Plateau of Southern India. The Vindhya Range is a complex chain of mountain ridges, hill ranges, highlands, and plateau escarpments in west-central India. The northern chain of the Vindhyas continues eastwards as Bhander Plateau and as the traditional boundary between Hindustan proper (North India) and Deccan (South India). The Vindhya Range lies in the north of the Satpura Range and the east of the Aravali range. The Amarkantak region is the meeting point of the Vindhya and the Satpura Ranges, with the Maikal Hills being the fulcrum. This is where the Narmada River, the Son River and Johila River emerge.

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The Vindhya Range separates the Indo-Gangetic Plains of Northern India from the Deccan Plateau of Southern India. The Vindhya Range is a complex chain of mountain ridges, hill ranges, highlands, and plateau escarpments in west-central India. The northern chain of the Vindhyas continues eastwards as Bhander Plateau and as the traditional boundary between Hindustan proper (North India) and Deccan (South India). The Vindhya Range lies in the north of the Satpura Range and the east of the Aravali range. The Amarkantak region is the meeting point of the Vindhya and the Satpura Ranges, with the Maikal Hills being the fulcrum. This is where the Narmada River, the Son River and Johila River emerge.

Karbi Anglong plateau is an extension of the Indian Karbi-Meghalaya Plateau or Indian Peninsular Plateau (Deccan Plateau) in Assam, a North Eastern state of India.

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Karbi Anglong plateau is an extension of the Indian Karbi-Meghalaya Plateau or Indian Peninsular Plateau (Deccan Plateau) in Assam, a North Eastern state of India.

Hojai district is situated between the Karbi Anglong Plateau and the Mikir Hills (now known as the Dima Hasao district).

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Hojai district is situated between the Karbi Anglong Plateau and the Mikir Hills (now known as the Dima Hasao district).

The Barail Range is situated in the southern part of Assam, forming a natural boundary between the Brahmaputra and Barak river basins.

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The Barail Range is situated in the southern part of Assam, forming a natural boundary between the Brahmaputra and Barak river basins.

The Hamren plateau is a part of the Karbi Anglong Plateau, which is an extension of the Peninsular Plateau. The Hamren sub-division of the Karbi Anglong district in Assam is continuous with the Meghalaya plateau.

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The Hamren plateau is a part of the Karbi Anglong Plateau, which is an extension of the Peninsular Plateau. The Hamren sub-division of the Karbi Anglong district in Assam is continuous with the Meghalaya plateau.

The Central Karbi Anglong Plateau is characterized by a radial drainage pattern. In this type of pattern, streams flow outward in all directions, like the spokes of a wheel, from a central high point (the plateau). This is a typical pattern for a relatively isolated upland area.

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The Central Karbi Anglong Plateau is characterized by a radial drainage pattern. In this type of pattern, streams flow outward in all directions, like the spokes of a wheel, from a central high point (the plateau). This is a typical pattern for a relatively isolated upland area.

The Dhansiri River forms a natural boundary between the Karbi Anglong Plateau and the Naga Hills. It originates in the Naga Hills and flows through Assam before joining the Brahmaputra River.

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The Dhansiri River forms a natural boundary between the Karbi Anglong Plateau and the Naga Hills. It originates in the Naga Hills and flows through Assam before joining the Brahmaputra River.

North East Extension Plateau

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North East Extension Plateau

Kaziranga National Park, a UNESCO World Heritage Site, is renowned for its diverse wildlife, particularly its large population of one-horned rhinoceroses. The Mora Diphlu River plays a crucial role in defining the park's southern boundary, contributing to its unique ecosystem.

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Kaziranga National Park, a UNESCO World Heritage Site, is renowned for its diverse wildlife, particularly its large population of one-horned rhinoceroses. The Mora Diphlu River plays a crucial role in defining the park's southern boundary, contributing to its unique ecosystem.