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Question 1 of 5
1. Question
Consider the following hills and their locations.
- Shevaroy Hills: Eastern Ghats
- Baba Budangiri Hills: Balaghat Range
- Cardamom Hills: Western Ghats
Which of the above pairs is/are correctly matched?
Correct
Solution: b)
Shevaroy Hills is one of the major hill stations in Tamil Nadu and in the Eastern Ghats.
Baba Budangiri is a mountain in the Baba Budan range of the Western Ghats of India.
The Cardamom Hills are mountain range of southern India and part of the southern Western Ghats located in southeast Kerala and southwest Tamil Nadu.
Incorrect
Solution: b)
Shevaroy Hills is one of the major hill stations in Tamil Nadu and in the Eastern Ghats.
Baba Budangiri is a mountain in the Baba Budan range of the Western Ghats of India.
The Cardamom Hills are mountain range of southern India and part of the southern Western Ghats located in southeast Kerala and southwest Tamil Nadu.
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Question 2 of 5
2. Question
In which of these regions, you are most likely to find a plant with breathing roots?
Correct
Solution: a)
Compared to other plants mangroves differ visually especially by their famous and typical aerial roots and biologically through the ability to grow in saline areas.
Aerial roots are roots with abilities such as enabling primary gas exchange in oxygen-poor soils.
Incorrect
Solution: a)
Compared to other plants mangroves differ visually especially by their famous and typical aerial roots and biologically through the ability to grow in saline areas.
Aerial roots are roots with abilities such as enabling primary gas exchange in oxygen-poor soils.
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Question 3 of 5
3. Question
What reasons can explain more number of debris avalanche in the Himalayas as compared to the Western Ghats?
- Himalayas are mostly made up of metamorphic and igneous rocks which are not stable.
- The Himalayas are tectonically active.
- The slopes are very steep in Himalayas as compared to Western Ghats.
Choose the correct answer using the codes below:
Correct
Solution: b)
In our country, debris avalanche and landslides occur very frequently in the Himalayas. There are many reasons for this. One, the Himalayas are tectonically active. They are mostly made up of sedimentary rocks and unconsolidated and semi-consolidated deposits. The slopes are very steep.
Compared to the Himalayas, the Nilgiris bordering Tamil Nadu, Karnataka, Kerala and the Western Ghats along the west coast are relatively tectonically stable and are mostly made up of very hard rocks; but, still, debris avalanches and landslides occur though not as frequently as in the Himalayas, in these hills due to very heavy rainfall.
Incorrect
Solution: b)
In our country, debris avalanche and landslides occur very frequently in the Himalayas. There are many reasons for this. One, the Himalayas are tectonically active. They are mostly made up of sedimentary rocks and unconsolidated and semi-consolidated deposits. The slopes are very steep.
Compared to the Himalayas, the Nilgiris bordering Tamil Nadu, Karnataka, Kerala and the Western Ghats along the west coast are relatively tectonically stable and are mostly made up of very hard rocks; but, still, debris avalanches and landslides occur though not as frequently as in the Himalayas, in these hills due to very heavy rainfall.
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Question 4 of 5
4. Question
Consider the following statements regarding Mountains
- Block Mountains are created when large areas are broken and displaced vertically.
- The uplifted blocks are termed as graben and the lowered blocks are called horsts.
- The Aravali range in India is one of the oldest block mountain systems in the world.
Which of the above statements is/are incorrect?
Correct
Solution: c)
There are three types of mountains- Fold Mountains, Block Mountains and the Volcanic Mountains. The Himalayan Mountains and the Alps are young fold mountains with rugged relief and high conical peaks. The Aravali range in India is one of the oldest fold mountain systems in the world. The range has considerably worn down due to the processes of erosion. The Appalachians in North America and the Ural mountains in Russia have rounded features and low elevation. They are very old fold mountains.
Block Mountains are created when large areas are broken and displaced vertically. The uplifted blocks are termed as horsts and the lowered blocks are called graben. The Rhine valley and the Vosges Mountain in Europe are examples of such mountain systems.
Incorrect
Solution: c)
There are three types of mountains- Fold Mountains, Block Mountains and the Volcanic Mountains. The Himalayan Mountains and the Alps are young fold mountains with rugged relief and high conical peaks. The Aravali range in India is one of the oldest fold mountain systems in the world. The range has considerably worn down due to the processes of erosion. The Appalachians in North America and the Ural mountains in Russia have rounded features and low elevation. They are very old fold mountains.
Block Mountains are created when large areas are broken and displaced vertically. The uplifted blocks are termed as horsts and the lowered blocks are called graben. The Rhine valley and the Vosges Mountain in Europe are examples of such mountain systems.
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Question 5 of 5
5. Question
Consider the following statements:
- Garo and Khasi hills are extensions of Purvanchals in Meghalaya forming water divide between Brahmaputra and Barak River.
- Rajmahal Hills are formed from rocks dating from the Jurassic Period and named after the town of Rajmahal which lies to the east in the state of Jharkhand.
Which of the above statements is/are incorrect?
Correct
Solution: a)
Garo and Khasi hills are the extensions of peninsular part of the subcontinent. Along with the Karbi Anglong plateau, the Meghalaya plateau (comprising Garo, Khasi and Jaintia hills) is separated from the Chotanagpur plateau (part of peninsular india ) by Malda fault (in Bengal).
Rajmahal Hills are formed from rocks dating from the Jurassic Period and named after the town of Rajmahal which lies to the east in the state of Jharkhand.
Incorrect
Solution: a)
Garo and Khasi hills are the extensions of peninsular part of the subcontinent. Along with the Karbi Anglong plateau, the Meghalaya plateau (comprising Garo, Khasi and Jaintia hills) is separated from the Chotanagpur plateau (part of peninsular india ) by Malda fault (in Bengal).
Rajmahal Hills are formed from rocks dating from the Jurassic Period and named after the town of Rajmahal which lies to the east in the state of Jharkhand.
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