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Question

Which of the following statements is/are correct?

1. Hypocenter is the point on the surface of the Earth, nearest to the focus.

2. Velocity of earthquake waves is higher in denser materials.

3. P waves move faster and are the first to arrive at the surface of the Earth.

Select the correct answer using the code given below:

This question was previously asked in
NDA I 2023 GAT Previous Year Paper (16-Apr-2023)
The correct answer is

2 and 3

Analyzing Statements on Earthquake Concepts

Let's carefully examine each statement provided regarding earthquakes and their associated phenomena.

Statement 1: Hypocenter and Epicenter Location

The statement says, "Hypocenter is the point on the surface of the Earth, nearest to the focus."

  • The focus (or hypocenter) is the point within the Earth where the earthquake rupture originates. This is where the seismic waves are generated.
  • The epicenter is the point on the surface of the Earth located directly above the focus (hypocenter). It is typically the area where the earthquake is felt most strongly.

Therefore, the statement is incorrect. The point on the surface nearest to the focus is the epicenter, not the hypocenter.

Statement 2: Velocity of Earthquake Waves in Denser Materials

The statement says, "Velocity of earthquake waves is higher in denser materials."

  • Seismic waves (P and S waves) travel through different materials within the Earth.
  • The speed of these waves depends on the properties of the material, specifically its density and rigidity (resistance to deformation).
  • Generally, seismic waves travel faster through denser and more rigid materials. For instance, waves travel faster through solid rock than through loose sediment or liquids.

Therefore, this statement is correct. The velocity of earthquake waves is indeed higher in denser and more rigid materials.

Statement 3: P Wave Speed and Arrival

The statement says, "P waves move faster and are the first to arrive at the surface of the Earth."

  • Earthquakes generate different types of seismic waves, including Body Waves (P waves and S waves) and Surface Waves.
  • P waves (Primary waves) are compressional waves. They travel through solids, liquids, and gases. They are the fastest type of seismic wave.
  • S waves (Secondary waves) are shear waves. They travel only through solids. They are slower than P waves.
  • Because P waves are the fastest, they are the first seismic waves to arrive at a seismograph station following an earthquake, regardless of whether it's on the surface or underground.

Therefore, this statement is correct. P waves move faster than other seismic waves and are the first to be detected at the Earth's surface.

Summary of Statement Analysis

Based on the analysis:

  • Statement 1: Incorrect (defines epicenter, not hypocenter).
  • Statement 2: Correct (wave velocity is higher in denser/more rigid materials).
  • Statement 3: Correct (P waves are fastest and arrive first).

The correct statements are 2 and 3.

Conclusion

The correct statements are Statement 2 and Statement 3.

Statement Correctness Reason
1. Hypocenter is the point on the surface nearest to the focus. Incorrect This describes the epicenter. Hypocenter is the focus within the Earth.
2. Velocity of earthquake waves is higher in denser materials. Correct Wave speed increases with density and rigidity.
3. P waves move faster and are the first to arrive. Correct P waves (Primary) are the fastest seismic waves.

Revision Table: Earthquake Terms & Waves

Term Definition
Focus (Hypocenter) The point within the Earth where the earthquake originates.
Epicenter The point on the Earth's surface directly above the focus.
P Waves (Primary Waves) Fastest seismic waves; compressional; travel through solids, liquids, gases.
S Waves (Secondary Waves) Slower than P waves; shear waves; travel only through solids.
Seismic Wave Velocity Speed depends on material properties (density, rigidity); faster in denser/more rigid materials.

Additional Information on Seismic Waves and Earth Structure

Understanding seismic waves is crucial for studying the Earth's interior. The way these waves travel and their speed changes provide geophysicists with information about the different layers of the Earth (crust, mantle, core).

  • Wave Refraction and Reflection: Seismic waves bend (refract) or bounce back (reflect) when they encounter boundaries between materials with different properties (like density or rigidity). This helps scientists map out layers within the Earth.
  • P and S Wave Travel Times: The difference in arrival times between P waves and S waves at a seismograph station can be used to calculate the distance from the station to the earthquake's epicenter.
  • Earthquake Magnitude and Intensity: Magnitude measures the energy released at the earthquake's source, while intensity measures the strength of shaking at a particular location, which depends on distance from the epicenter, local geology, and building construction.

By studying these waves, scientists can locate earthquakes, understand their causes, and learn about the structure and composition of the Earth's deep interior.

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