Questions Related to geography

Multiple choice geography our changing earth earthquake and volcanoes earthquake earthquakes

The point of origin of waves of earthquake is called as ________________.

  1. Seismic focus

  2. Seismic line

  3. Seismic centre

  4. None of these

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

The Focus or Seismic Focus is also called the hypocenter of an earthquake. The vibrating waves travel away from the focus of the earthquake in all directions. The waves can be so powerful they will reach all parts of the Earth and cause it to vibrate like a tuning fork. The focus is the exact point inside the crust of the earth where the quake begins.

Multiple choice geography our changing earth earthquake and volcanoes earthquake earthquakes

In 1906 San Andreas Fault of California gave rise to major earthquake because of __________.

  1. plate tectonic

  2. folding and faulting

  3. volcanic activity

  4. none of these

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

The San Andreas Fault is a transform plate boundary where the movement of tectonic plates causes folding and faulting of the Earth's crust, leading to earthquakes.

Multiple choice geography our changing earth earthquake and volcanoes earthquake earthquakes

The vibration of earthquakes, last from a few seconds to several minutes, called as ______.

  1. duration

  2. period

  3. hour

  4. none of these

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

Duration is the vibration of earthquakes which can be felt by human beings that last from a few seconds to several minutes. Generally, the greater the intensity of the shocks, the longer they last. The average duration of shocks of sufficient intensity to produce much damage is perhaps from one to two minutes.

Multiple choice geography our changing earth earthquake and volcanoes earthquake earthquakes

There are annually 8,000-10,000 earthquakes in the world, which comes to about an earthquake every hour known as, ____________.

  1. Earthquake velocity

  2. Earthquake frequency

  3. Earthquake wave

  4. None of these

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

There are annually 8,000 - 10,000 earthquakes in the world, which comes to about an earthquake every hour. And there are many more that go undetected because there are no stations to record them over the oceans covering a very large surface of our earth. This is known as the Earthquake Frequency

Multiple choice geography our changing earth earthquake and volcanoes earthquake earthquakes

A line connecting all points on the surface of the earth where the intensity of shock produced by earthquake waves is the same.

  1. Isosismic line

  2. Isohyte lines

  3. Isobars

  4. Isotherm lines

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

Isoseismic Line is the line connecting all points on the surface of the earth where the intensity is the same. These lines show great irregularity in their form. 

Multiple choice geography our changing earth earthquake and volcanoes earthquake earthquakes

Find the odd one out and give explanation for your choice.

  1. Tectonics

  2. Centrifugal Force

  3. Solar energy

  4. Precipitation

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

Tectonics is a geological process involving the Earth's crust, whereas centrifugal force, solar energy, and precipitation are atmospheric or physical forces related to weather and climate.

Multiple choice geography our changing earth earthquake and volcanoes earthquake earthquakes

The most destructive earthquake waves are ___________.

  1. primary waves

  2. secondary waves

  3. surface waves

  4. all of these

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

During an earthquake, surface waves are the seismic waves that cause the most damage. Unlike other seismic waves that move deep inside the Earth, surface waves move along just under the surface of the Earth like waves in water. Surface waves are the slowest seismic waves and are the final waves to hit an area after an earthquake. First, P-waves move through compression through the deep layers of the Earth. They result in minimal damage. The second group of waves is S-waves. They move up and down starting deeper in the Earth. Stronger S-waves do some damage when they reach the surface. Surface waves move in last. Their slow roll just under the surface provides the greatest risk for damage to man-made structures and changes to natural landforms