geomorphology & earth landforms section 1 MCQ Questions & Answers Detailed Explanation
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The following question based on Geomorphology & Earth landforms topic of indian geography mcq
- Block mountains: These are originated by tensile forces leading to the formation of rift valleys. They are also called as Horst Mountains.
- Dome mountains: These are formed due to the accumulation of volcanic materials. Different types of volcanic cones (e. g. cinder cones, composite cones, basic lava cones, etc.) come under this category
- Mountains of Accumulations: These are originated from magmatic intrusions and up warping of the crustal surface. Examples are Normal domes, lava domes, batholithic domes, laccolithic domes, salt domes.
(a) 1 and 3
(b) 1 only
(c) 1, 2 and 3
(d) 2 and 3
The correct answers to the above question in:
Answer: (b)
Block mountains:These are originated by tensile forces leading to the formation of rift valleys. They are also called as horst mountains.
Dome mountains: These are originated by magmatic intrusions and upwarping of the crustal surface. Examples are: Normal domes, lava domes, batholithic domes, laccolithic domes, salt domes.
Mountains of Accumulations:These are formed due to accumulation of volcanic materials. Different types of volcanic cones (e. g. cinder cones, composite cones, basic lava cones, etc.) come under this category.
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Read more geomorphology earth landforms Based Indian Geography Questions and Answers
Question : 1
Winds blowing constantly in one direction in rocky deserts form
a) Yardangs
b) Chimneys
c) Demoiselles
d) Mushrooms rocks
Answer »Answer: (a)
In regions of rocky deserts, wind abrasion excavates the bands of softer rocks into long, narrow corridors, separating the steep-sided over-hanging ridges of hard rocks, called yardangs.
Instead of lying in horizontal strata upon one another, the hard and soft rocks of yardangs are vertical bands and are aligned in the direction of the prevailing winds.
Question : 2
Suppose if we measure the time lapse between the two Sunsets by sitting in the beach, from this we can estimate
a) The radius of the earth
b) The distance between the sun and the earth
c) The radius of the sun
d) The depth of the ocean
Answer »Answer: (a)
A method is described whereby, using primitive equipment anyone can measure the size of the earth to an accuracy of order of magnitude 10% by observing two sunsets in the space of a few seconds.
Question : 3
Consider the following statements :
- The Terai region is made up of stones and pebbles. It is so highly porous that rivers disappear in the region.
- In the Bhabhar region, rivers re-emerge and this region is very marshy. This is a region of dense forests and high biological diversity.
- Khadar region is made up of new alluvium.
- Bhangar region is made up of new alluvium.
a) 2 and 3
b) 1 and 2
c) 1, 2 and 3
d) 2 only
Answer »Answer: (a)
Bhabhar Region This region is found along the foothills of Shivalik from Indus to Tista without any break.
Since it is made up of stones and pebbles, it is so highly porous that rivers disappear in this region.
Terai Region This region is found to the South of the Bhabhar region. Due to the very high humidity caused due to the reemergence of rivers, this region is very marshy. The speed of river flow in this region is slow. This is a region of dense forests and high biological diversity. Khadar Region It is made up of new alluvium.
In this region, floods bring new alluvium every year. Bhangar Region It is that higher part of the plains, where the floodwater cannot reach. It is made up of old alluvium.
Question : 4
Which of the following range of mountains is not the result of Tertiary orogeny?
a) Alps
b) Kunlun
c) Andes
d) Applachians
Answer »Answer: (d)
Question : 5
What was the period of the Dinosaurs?
a) Forty crore years ago
b) Five crore years ago
c) Eighty crore years ago
d) Eighteen crore years ago
Answer »Answer: (b)
Question : 6
The inner-most layer of the earth is known as
a) Asthenosphere
b) Lithosphere
c) Barysphere
d) Mesosphere
Answer »Answer: (a)
The inner core is the innermost physical layer of the Earth. The asthenosphere is the highly viscous, mechanically weak and ductilely-deforming region of the upper mantle of the Earth.
It lies below the lithosphere, at depths between 100 and 200 km below the surface, but perhaps extending as deep as 700 km.
GET Geomorphology & Earth landforms PRACTICE TEST EXERCISES
geomorphology & earth landforms section 1
geomorphology & earth landforms section 2
geomorphology & earth landforms section 3
geomorphology & earth landforms section 4
geomorphology & earth landforms section 5
geomorphology & earth landforms section 6
geomorphology & earth landforms section 7
geomorphology & earth landforms section 8
geomorphology & earth landforms section 9
geomorphology & earth landforms section 10
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