Physical Features of India

Rivers like Mahanadi Godavari Krishna and Kaveri cut across Eastern Ghats. For exams remember Eastern Ghats as discontinuous.

Nilgiri is related to the contact zone of Western and Eastern Ghats. For exams identify it on the southern mountain map.

Anamudi and Doddabetta are separate mountain identities of South India. For exams remember the peak and range relation.

The eastern coast is broad and large rivers deposit silt near Bay of Bengal. For exams remember Mahanadi Godavari Krishna Kaveri.

Western Ghats are close to the sea so the western coast is narrow and rivers are short. For exams remember the east west coast comparison.

The direct answer is A: Konkan, Kannad and Malabar are parts of the western coastal plain arranged broadly from north to south. A coastal plain is the low land beside a sea. India’s western coastal plain lies between the Arabian Sea and the Western Ghats and is divided into regional sections. Step by step: identify the three names; place them on the western, Arabian Sea side of India; read their broad north-to-south sequence; conclude that they describe the western coastal division. Option A is correct. Option B is wrong because the eastern coastal plain is associated with broad deltas of rivers such as the Mahanadi, Godavari, Krishna and Kaveri, not this sequence. Option C concerns Himalayan height zones, far from the coast. Option D concerns desert dunes in the Thar, also unrelated. The exact naming can vary slightly between textbooks, but the intended school-geography classification is clearly the western coastal plain. Memory cue: Arabian Sea side—Konkan, Kannad, Malabar.

Northern Circars and Coromandel are linked with India's eastern coastal plain. For exams connect them with Bay of Bengal.

Barchans are desert landforms formed by wind transport and deposition of sand. For exams remember aeolian action.

Luni is linked with a dry region and does not form a clear marine delta. For exams remember the Luni and Thar relation.

When water dries in the Rann salt remains on the surface. For exams remember Rann of Kachchh as a saline plain.

Ladakh is cold and dry due to altitude and Himalayan rain shadow. For exams remember the cause of cold desert.

Lakshadweep is a coral island group and Barren Island is a volcanic example in Andaman. For exams keep island origins separate.

Majuli is a river island Sundarbans is a delta and Lakshadweep is a coral island. For exams keep landform types separate.

Indira Point is in Nicobar while Kanyakumari is on the mainland. For exams keep southernmost point and mainland southern tip separate.

Palk Strait is a shallow sea passage between Tamil Nadu and Sri Lanka. For exams identify it on the map.

Moist winds hit Khasi Hills rise upward and cause heavy rainfall. For exams remember the Meghalaya and orographic rainfall relation.

Thar is a hot dry desert while Ladakh is a cold desert due to altitude and rain shadow. For exams keep them separate.

The Deccan region shows a clear relation between basaltic lava and black soil. For exams remember Deccan cotton and black soil.

The direct answer is A, Bhabar to Terai. In the Himalayan foothill region, the Bhabar belt is made of coarse pebbles, gravel, and porous material. River water often sinks into this highly permeable belt. Further south, the water reappears and creates the wetter, marshy Terai belt. Option A is correct because it gives this exact geographical sequence: porous pebbly Bhabar followed by moist marshy Terai. Option B, Khadar to Bhangar, describes two types of alluvial plains, not the pebbly-to-marshy foothill sequence; also, their order and features do not match here. Option C, Konkan to Malabar, names coastal regions and does not describe Himalayan belts. Option D, Thar to Ladakh, joins two different dry or high-altitude regions and has no such sequence. The fact chain is: Himalayan foothills → coarse porous Bhabar → underground flow → wet marshy Terai. Memory cue: Bhabar hides the water; Terai brings the water back and becomes marshy.

Bhabar is a pebbly porous foothill belt of the Himalayas not a tidal marsh. For exams keep Bhabar and Sundarbans separate.

Sundarbans is the tidal saline mangrove area of Ganga Brahmaputra Delta. For exams identify this clue quickly.

Narmada flows west through a rift valley into Arabian Sea. For exams remember Narmada Tapi as special exceptions.

The origin of a landform means the natural process through which it was created. The Deccan Trap is a vast volcanic formation produced by successive outpourings of lava. After cooling, the lava formed layers of basaltic rock. Lakshadweep has a contrasting origin: its islands developed from coral growth and the accumulation of coral material in warm, shallow tropical seas. Thus, the two examples display volcanic and coral origins together.

Option A is correct because it gives the clearest contrast in geological formation. Khadar and Bhangar are both varieties of river-laid alluvium, although one is newer and the other older. Konkan and Malabar are coastal regions, and Chambal and Betwa are rivers. Their pairing does not show two such distinct origins.

India has many types of landforms that create its physical diversity. For exams study major physical divisions on a map.

Rivers originating from the Himalayas deposit alluvium in the plains. For exams study mountains rivers and plains as one sequence.