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Question 1 of 5
1. Question
Consider the following statements regarding Plate tectonics.
- The driving force behind plate tectonics is convection in the mantle.
- At transform boundaries, crust is neither produced nor destroyed as the plates slide horizontally past each other.
- The Mid-Atlantic Ridges are a good example of convergent boundary.
How many of the above statements are correct?
Correct
Solution: b)
Statement 3 is incorrect.
There are four types of plate boundaries:
- Divergent boundaries — where new crust is generated as the plates pull away from each other.
- Convergent boundaries — where crust is destroyed as one plate dives under another.
- Transform boundaries — where crust is neither produced nor destroyed as the plates slide horizontally past each other.
- Plate boundary zones — broad belts in which boundaries are not well defined and the effects of plate interaction are unclear.
Divergent boundaries occur along spreading centers where plates are moving apart and new crust is created by magma pushing up from the mantle. Picture two giant conveyor belts, facing each other but slowly moving in opposite directions as they transport newly formed oceanic crust away from the ridge crest.
Perhaps the best known of the divergent boundaries is the Mid-Atlantic Ridge.
Incorrect
Solution: b)
Statement 3 is incorrect.
There are four types of plate boundaries:
- Divergent boundaries — where new crust is generated as the plates pull away from each other.
- Convergent boundaries — where crust is destroyed as one plate dives under another.
- Transform boundaries — where crust is neither produced nor destroyed as the plates slide horizontally past each other.
- Plate boundary zones — broad belts in which boundaries are not well defined and the effects of plate interaction are unclear.
Divergent boundaries occur along spreading centers where plates are moving apart and new crust is created by magma pushing up from the mantle. Picture two giant conveyor belts, facing each other but slowly moving in opposite directions as they transport newly formed oceanic crust away from the ridge crest.
Perhaps the best known of the divergent boundaries is the Mid-Atlantic Ridge.
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Question 2 of 5
2. Question
Consider the following statements regarding the difference(s) between extrusive and intrusive rocks?
- Extrusive rocks are fine grained, whereas intrusive rocks are coarse-grained.
- Extrusive rocks form over a much longer duration of time compared to intrusive rocks.
Which of the above statements is/are correct?
Correct
Solution: a)
The key difference between intrusive and extrusive rocks is that the intrusive rocks are formed from magma whereas the extrusive rocks are formed from lava.
Intrusive rocks: With no air to cool the magma, these rocks are formed very slowly. Composition of these rocks reflects presence of large crystals. These crystals interlock to form the rock.
These rocks take a very large amount of time to solidify and they remain buried deep inside the surface of the earth being surrounded by country rocks that have been there already.
Very slow cooling means that these rocks remain coarse-grained.
Some of the perfect examples of intrusive rocks are the diorite, gabbro, and granite.
Much of the core of various mountain ranges around the world is made up of these intrusive rocks.
Extrusive Rocks: Sometimes, molten rocks find a way to come out of the surface of the earth through cracks and openings.
This magma flows in the form of lava and cools down quickly as it comes into contact with air.
Igneous rocks that are formed from the magma that pours out of the surface of the earth are called extrusive rocks.
As these rocks cool down and solidify very quickly, they do not get sufficient time to form large crystals. Thus, they have small crystals and boast a fine texture.
Incorrect
Solution: a)
The key difference between intrusive and extrusive rocks is that the intrusive rocks are formed from magma whereas the extrusive rocks are formed from lava.
Intrusive rocks: With no air to cool the magma, these rocks are formed very slowly. Composition of these rocks reflects presence of large crystals. These crystals interlock to form the rock.
These rocks take a very large amount of time to solidify and they remain buried deep inside the surface of the earth being surrounded by country rocks that have been there already.
Very slow cooling means that these rocks remain coarse-grained.
Some of the perfect examples of intrusive rocks are the diorite, gabbro, and granite.
Much of the core of various mountain ranges around the world is made up of these intrusive rocks.
Extrusive Rocks: Sometimes, molten rocks find a way to come out of the surface of the earth through cracks and openings.
This magma flows in the form of lava and cools down quickly as it comes into contact with air.
Igneous rocks that are formed from the magma that pours out of the surface of the earth are called extrusive rocks.
As these rocks cool down and solidify very quickly, they do not get sufficient time to form large crystals. Thus, they have small crystals and boast a fine texture.
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Question 3 of 5
3. Question
Valuable minerals in India are more likely to be associated with
Correct
Solution: b)
Quartz and Basalt both can be associated with sedimentary rocks, even though Quartz may occur in felsic igneous rocks or granite.
Bulk of the valuable minerals in India are products of pre-Palaeozoic age spanning from nearly 540-250 million years ago. Hadean age refers to the one right after formation of earth.
These minerals are mostly associated with metamorphic and igneous rocks of the peninsular India, and not sedimentary rocks.
Incorrect
Solution: b)
Quartz and Basalt both can be associated with sedimentary rocks, even though Quartz may occur in felsic igneous rocks or granite.
Bulk of the valuable minerals in India are products of pre-Palaeozoic age spanning from nearly 540-250 million years ago. Hadean age refers to the one right after formation of earth.
These minerals are mostly associated with metamorphic and igneous rocks of the peninsular India, and not sedimentary rocks.
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Question 4 of 5
4. Question
Which of the following are block mountains:
- The Vosges mountain
- Satpura Mountains
- Mount Kilimanjaro
Select the correct answer code:
Correct
Solution: a)
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. Vindhyan and Satpura ranges with Narmada rift valley is another example.
Volcanic mountains are formed due to volcanic activity. Mt.Kilimanjaro in Africa and Mt.Fujiyama in Japan are examples of such mountains.
Incorrect
Solution: a)
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. Vindhyan and Satpura ranges with Narmada rift valley is another example.
Volcanic mountains are formed due to volcanic activity. Mt.Kilimanjaro in Africa and Mt.Fujiyama in Japan are examples of such mountains.
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Question 5 of 5
5. Question
Ladakh, a cold desert in the Greater Himalayas, is enclosed by
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