Geography · General Awareness

Geology and Earth Structure

1,345 Questions

Geology and Earth Structure explores the physical composition of the planet, including its layers, tectonic plates, and seismic activity. This topic is a core component of geography and general science sections in various competitive exams. Reviewing these concepts builds a solid foundation for answering questions related to natural phenomena.

Layers of the EarthTectonic PlatesEarthquakes and VolcanoesGeomagnetism ApplicationsGeophysical MethodsLandform Formation

Geology and Earth Structure Questions

Multiple choice
  1. Chota Nagpur Plateau

  2. Deccan Plateau

  3. Vindhyan Plateau

  4. Dandakaranya region

Reveal answer Fill a bubble to check yourself
B Correct answer
Explanation

The Maharashtra Plateau or Deccan Plateau was formed in the cretaceous period due to massive upheaval of basaltic lava from the interior of the earth. It has gentle slope in the South (towards the Karnataka Plains) and steep slope in the North (towards the Satpura ranges).

Multiple choice
  1. volcanic eruptions

  2. meteor hits

  3. underground nuclear explosions

  4. movement of earth’s plates

Reveal answer Fill a bubble to check yourself
D Correct answer
Explanation

Most of the earthquakes are caused by the movement of earth’s plates.

Multiple choice
  1. Whole of the south India is not prone to earthquakes.

  2. Only western and central Himalayas are earthquake-prone with the whole of northeast being danger free.

  3. Rann of Kutch and Rajasthan are not earthquake-prone.

  4. The Indo-gangetic plane is earthquake-prone.

Reveal answer Fill a bubble to check yourself
D Correct answer
Explanation

The Indo-gangetic plane is earthquake-prone. Only option (4) is correct. 

Multiple choice

The passage says that early instruments for measuring earthquakes were

Directions: Read the following passage and answer the given question.

An earthquake comes like a thief in the night, without warning. It was necessary, therefore, to invent instruments that neither slumbered nor slept. Some devices were quite simple. One, for instance, consisted of rods of various lengths and thicknesses which would stand up on end like ninepins. When a shock came it shook the rigid table upon which these stood. If it were gentle, only the more unstable rods fell. If it were severe, they all fell. Thus, the rods by falling and by the direction in which they fell, recorded for the slumbering scientist, the strength of a shock that was too weak to waken him and the direction from which it came.

But, instruments far more delicate than that were needed if any really serious advance was to be made. The ideal to be aimed at was to devise an instrument that could record with a pen on paper the movements, of the ground or of the table, as the quake passed by. While I write, my pen moves but the paper keeps still. With practice, no doubt, I could, in time, learn to write by holding the pen still while the paper moved. That sounds a silly suggestion, but that was precisely the idea adopted in some of the early instruments (seismometers) for recording earthquake waves. But when table, penholder and paper are all moving, how is it possible to write legibly? The key to a solution of that problem lay in an everyday observation. Why does a person standing in a bus or train tend to fall when a sudden start is made? It is because his feet move on, but his head stays still.

  1. faulty in design

  2. expensive

  3. not sturdy

  4. not sensitive enough

Reveal answer Fill a bubble to check yourself
D Correct answer
Explanation

"But, instruments far more delicate than that were needed..."

Multiple choice

The early seismometers adopted the idea that in order to record the earthquake, it is

Directions: Read the following passage and answer the given question.

An earthquake comes like a thief in the night, without warning. It was necessary, therefore, to invent instruments that neither slumbered nor slept. Some devices were quite simple. One, for instance, consisted of rods of various lengths and thicknesses which would stand up on end like ninepins. When a shock came it shook the rigid table upon which these stood. If it were gentle, only the more unstable rods fell. If it were severe, they all fell. Thus, the rods by falling and by the direction in which they fell, recorded for the slumbering scientist, the strength of a shock that was too weak to waken him and the direction from which it came.

But, instruments far more delicate than that were needed if any really serious advance was to be made. The ideal to be aimed at was to devise an instrument that could record with a pen on paper the movements, of the ground or of the table, as the quake passed by. While I write, my pen moves but the paper keeps still. With practice, no doubt, I could, in time, learn to write by holding the pen still while the paper moved. That sounds a silly suggestion, but that was precisely the idea adopted in some of the early instruments (seismometers) for recording earthquake waves. But when table, penholder and paper are all moving, how is it possible to write legibly? The key to a solution of that problem lay in an everyday observation. Why does a person standing in a bus or train tend to fall when a sudden start is made? It is because his feet move on, but his head stays still.

  1. the pen that should move just as it moves when we write on paper

  2. the pen that should stay still and the paper should move

  3. both the pen and the paper that should move

  4. neither the pen nor the paper that should move

Reveal answer Fill a bubble to check yourself
B Correct answer
Explanation

"While I write, my pen moves but the paper keeps still." 

Multiple choice

Why was it necessary to invent instruments to observe an earthquake?

Directions: Read the following passage and answer the given question.

An earthquake comes like a thief in the night, without warning. It was necessary, therefore, to invent instruments that neither slumbered nor slept. Some devices were quite simple. One, for instance, consisted of rods of various lengths and thicknesses which would stand up on end like ninepins. When a shock came it shook the rigid table upon which these stood. If it were gentle, only the more unstable rods fell. If it were severe, they all fell. Thus, the rods by falling and by the direction in which they fell, recorded for the slumbering scientist, the strength of a shock that was too weak to waken him and the direction from which it came.

But, instruments far more delicate than that were needed if any really serious advance was to be made. The ideal to be aimed at was to devise an instrument that could record with a pen on paper the movements, of the ground or of the table, as the quake passed by. While I write, my pen moves but the paper keeps still. With practice, no doubt, I could, in time, learn to write by holding the pen still while the paper moved. That sounds a silly suggestion, but that was precisely the idea adopted in some of the early instruments (seismometers) for recording earthquake waves. But when table, penholder and paper are all moving, how is it possible to write legibly? The key to a solution of that problem lay in an everyday observation. Why does a person standing in a bus or train tend to fall when a sudden start is made? It is because his feet move on, but his head stays still.

  1. Because an earthquake comes like a thief in the night

  2. To make people alert about earthquakes during their conscious as well as unconscious hours

  3. To prove that we are technically advanced

  4. To experiment with the control of man over nature

Reveal answer Fill a bubble to check yourself
B Correct answer
Explanation

"It was necessary, therefore, to invent instruments that neither slumbered nor slept."

Multiple choice
  1. oxygen and iron

  2. silicon and magnesium

  3. silicon and aluminum

  4. oxygen and silicon

Reveal answer Fill a bubble to check yourself
D Correct answer
Explanation

Oxygen (46-47%) and silicon (27-28%) are the two most abundant elements in Earth's crust by mass. Oxygen is found in silicates, oxides, and water. Silicon is the second most abundant and is the foundation of silicate minerals that make up most rocks. Options A, B, and C are incorrect because while iron, magnesium, and aluminum are abundant, they rank below oxygen and silicon. Aluminum is actually the third most abundant (~8%), followed by iron (~5%) and calcium (~3.6%).