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The two coastal strips flanking the Peninsular Plateau are along the Arabian Sea on the west and the Bay of Bengal on the east.
The northern part of the western coast is called the Konkan.
The western coastal plain lies between the Western Ghats and the Arabian Sea.
The central stretch of the western coast is known as the Kannad Plain.
The southern stretch of the western coast is referred to as the Malabar coast.
The largest saltwater lake in India is Chilika Lake.
Chilika Lake is located in the state of Odisha.
Khadar refers to newer, younger deposits of the floodplains that are fertile and ideal for intensive agriculture.
The Peninsular Plateau is composed of old crystalline, igneous, and metamorphic rocks.
The Peninsular Plateau was formed due to the breaking and drifting of the Gondwana land.
The youthful topography of the Peninsular Plateau consists of high peaks, deep valleys, and fast-flowing rivers.
The northern plains of India are formed of alluvial deposits.
The Peninsular Plateau contains igneous and metamorphic rocks.
The coastal plains are significant for their fertile land and agricultural potential due to the deposition of alluvial soil.
The Konkan region has fertile coastal plains that support various agricultural activities.
The Malabar coast is famous for its backwaters and lagoons.
The Kannad Plain is important for agriculture due to its fertile land and favorable climate.
The coastal plains of India are affected by monsoon winds, making them suitable for diverse agriculture.
Coastal plains support a rich biodiversity due to their varied ecosystems, including wetlands and coastal forests.
The geography of the coastal plains, with their fertile land and access to water, makes them attractive for human settlement and agriculture.