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Subjects

Geography

The Coastal Plains and Islands

In this Class 9 Geography topic from Physical Features of India, students explore how India’s coastal plains and islands were formed and how they differ in location, relief, and physical features. They study the Western Coastal Plain along the Arabian Sea and the broader Eastern Coastal Plain along the Bay of Bengal, including important rivers, deltas, lagoons, and coastal processes. The topic also introduces the Andaman and Nicobar Islands and Lakshadweep, highlighting their geographical setting, natural environment, and importance to India.

Hard · Level 2 · 25 questions

TOPIC PRACTICE

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25 questions

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  1. Shallow water bodies partly separated from the sea
  2. Deep valleys formed by mountain glaciers
  3. Sand dunes made by desert winds
  4. Plateaus made by seismic waves
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  1. Limited space between the sea and Western Ghats
  2. Very long distance between Eastern Ghats and Himalayas
  3. Absence of the Ganga delta
  4. Permanent effect of snowy climate
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  1. Eastern coast rivers form large deltas while many western coast rivers form estuaries
  2. All western coast rivers originate in the Himalayas
  3. There is no permanent river on the eastern coast
  4. Only coral rivers are found on both coasts
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  1. Broad alluvial plains made by long rivers
  2. Chain of coral islands
  3. Indented rocky western coast
  4. Abundance of glacial lakes
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  1. Fertile deltaic soil and water availability
  2. Hard surface of coral reefs
  3. High slope of lava plateau
  4. Dry sand and saline groundwater
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  1. Availability of sea, bays, mouths and lagoons
  2. High glaciers and snowy peaks
  3. Spread of sandy desert
  4. Deep inland trenches
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  1. They affect maritime boundary, biodiversity and strategic location
  2. They completely remove India's plains
  3. They only create Himalayan climate
  4. They are the origin of all rivers
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  1. Tropical island climate and marine ecology
  2. Continuous snowfall and polar climate
  3. Complete desert environment
  4. Flat alluvial land of the Ganga plain
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  1. Coral reefs are fragile ecosystems
  2. They are hard mountains made of Himalayan rocks
  3. They are formed every year by Ganga floods
  4. They are at the centre of an inland plateau
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  1. The possibility of large deltas remains low
  2. Every river forms a huge delta
  3. Glaciers form at river mouths
  4. Rivers do not flow towards the sea
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  1. Deltas and sediment deposition may make waterways shallow
  2. There is complete absence of sea
  3. Glaciers spread over the whole coast
  4. All rivers flow westward
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  1. Agriculture, fishing, trade and port activities
  2. Only glacier tourism
  3. Only desert camel trade
  4. Only inland mining
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  1. They change coastline shape, sand bars and lagoons
  2. They immediately increase the height of the Himalayas
  3. They make all rivers underground
  4. They turn deserts into seas
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  1. Broad and fertile alluvial coastal plain
  2. High and continuous mountainous coast
  3. Closed chain of coral reefs
  4. Group of glacial valleys
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  1. Small area and sea water can make groundwater limited and sensitive
  2. It never rains on islands
  3. All islands are covered by glaciers
  4. Sea water is always fresh
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  1. Sediment deposition at river mouth and influence of sea tides
  2. Height of mountain peak
  3. Complete absence of rainfall
  4. Colour of vegetation
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  1. Partial separation of sea water by sand bars
  2. Formation of mountain peaks by lava
  3. Downward movement of glaciers
  4. Deposition of desert dust
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  1. Western Ghats quickly force moist sea winds upward
  2. Eastern Ghats stop the Arabian Sea
  3. Bay of Bengal completely dries the western coast
  4. There is no mountain effect on the coast
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  1. Shallow deltaic coast and sediment deposition can hinder ships
  2. Deltas always create very deep seas
  3. There are no sea waves on the eastern coast
  4. Eastern Ghats are located inside the sea
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  1. It is an island group in the sea with distinct origin and ecology
  2. It is an inner part of the Ganga plain
  3. It is a plain of the Western Ghats
  4. It is an extension of the Thar Desert
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  1. Northern Circar and Coromandel
  2. Konkan and Malabar
  3. Kanara and Kathiawar
  4. Lakshadweep and Minicoy
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  1. Eastern Coastal Plain
  2. Narrow backwater region of Malabar
  3. Dry coastal part of Kachchh
  4. Coral island of Lakshadweep
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  1. It explains the relation of land, sea, river deposition and island ecology
  2. It only measures the height of the Himalayas
  3. It only explains desert climate
  4. It proves all Indian rivers flow northward
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  1. The Western Ghats run very close and almost parallel to the Arabian Sea
  2. The Eastern Ghats are connected with the Himalayas
  3. No river drains into the Arabian Sea
  4. Only deltas are formed on the western coast
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  1. Large east-flowing rivers deposit sediments on a broad plain and shallow coast
  2. The Eastern Ghats are very high and continuous
  3. The Bay of Bengal has no tides
  4. Rivers on the eastern coast are very short

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