Question map
Consider the following statements : 1. In a seismograph, P waves are recorded earlier than S waves. 2. In P waves, the individual particles vibrate to and fro in the direction of wave propagation whereas in S waves, the particles vibrate up and down at right angles to the direction of wave propagation. Which of the statements given above is/are correct?
Explanation
The correct answer is Option 3 (Both 1 and 2) because both statements accurately describe the physical properties of seismic waves.
- Statement 1 is correct: P-waves (Primary waves) are longitudinal waves that travel faster than S-waves (Secondary waves). Due to their higher velocity, P-waves are the first to be detected and recorded by a seismograph after an earthquake occurs, followed by the slower S-waves.
- Statement 2 is correct: This describes the particle motion of each wave type. P-waves are compressional; particles vibrate parallel (to and fro) to the direction of energy propagation. In contrast, S-waves are transverse; particles move perpendicular (up and down or side to side) to the wave's path.
Since P-waves always precede S-waves and their respective vibration patterns are correctly identified, both statements are scientifically sound, making Option 3 the right choice.
PROVENANCE & STUDY PATTERN
Full viewThis is a classic 'bread and butter' question directly from NCERT Class XI (Fundamentals of Physical Geography). It is a high-fairness static question. If you get this wrong, you are at a severe disadvantage because the 'serious crowd' will mark this with 100% accuracy. No current affairs linkage required.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: In a seismograph recording, are P waves recorded earlier than S waves?
- Statement 2: In seismology, do particles in P waves vibrate to-and-fro in the direction of wave propagation (i.e., are P waves longitudinal)?
- Statement 3: In seismology, do particles in S waves vibrate at right angles to the direction of wave propagation (i.e., are S waves transverse)?
- Explicitly states P-waves are the fastest seismic waves and therefore are recorded first on the seismograph.
- Describes P-waves as longitudinal/compressional waves whose transmission properties explain their rapid arrival.
- Labels S-waves as 'secondary' and notes they are recorded second on the seismograph.
- Explicitly states S-waves arrive at the surface after the P-waves and are transverse (shear) in nature.
- Provides a quantitative speed relation: P-waves are about 1.7 times faster than S-waves.
- Explains the physical reason (compression waves transmit energy more quickly than shear waves), supporting earlier arrival of P-waves.
- Explicitly labels primary (P) waves as 'longitudinal' and equates this with particle displacement parallel to the wave direction.
- Describes P-waves as compressional/pressure waves that produce compression and rarefaction along propagation.
- Directly states P-waves vibrate parallel to the direction of the wave (to-and-fro along propagation).
- Explains resulting stretching and squeezing (density differences) in the material along the propagation direction.
- Describes P-waves as compression waves applying force in the direction of propagation.
- Links this compressional motion to efficient energy transmission and higher speed relative to S-waves.
- Explicitly names S-waves 'transverse'/'shear' and equates transverse with particle motion perpendicular to propagation.
- States that transverse waves cause troughs and crests by perpendicular vibrations, matching the definition in the question.
- Describes S-waves as transverse/shear and specifies motion of the medium is perpendicular to propagation.
- Contrasts with P-waves to reinforce the perpendicular nature of S-wave particle motion.
- States S-wave vibrations are perpendicular to wave direction (in the vertical plane).
- Groups S-waves with other waves that vibrate perpendicular, reinforcing the transverse classification.
- [THE VERDICT]: Absolute Sitter. Source: NCERT Class XI Fundamentals of Physical Geography, Chapter 3 (Interior of the Earth).
- [THE CONCEPTUAL TRIGGER]: Geomorphology > Earth's Interior > Body Waves (P & S) vs Surface Waves (L & R).
- [THE HORIZONTAL EXPANSION]: Memorize the Shadow Zones: P-wave shadow is a band (105Β°-145Β°), S-wave shadow is a massive zone (>105Β°). Know the medium rules: P travels through Solid/Liquid/Gas (fastest in solid), S only through Solids. Know the destructiveness order: Surface Waves > S-waves > P-waves.
- [THE STRATEGIC METACOGNITION]: Do not skim the 'science' parts of Geography. The distinction between Longitudinal (Sound-like) and Transverse (Light-like/Ripples) waves is basic physics that UPSC loves to test in Geography. Visualizing the particle motion (push-pull vs up-down) is essential.
P-waves travel faster and are recorded before S-waves on seismographs.
High-yield for earthquake seismology questions: knowing arrival order is essential to reading seismograms and calculating epicentral distance. Connects to locating epicentres and interpreting seismic records in physical geography and geology questions.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Primary Waves (P-Waves) > p. 60
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Secondary Waves (S-Waves) > p. 62
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Why Do P-Waves Travel Faster Than S-Waves? > p. 61
P-waves are compressional (longitudinal) waves that transmit energy rapidly through materials.
Important for explaining why P-waves reach stations first and for understanding seismic wave propagation through different layers; links to questions on wave types, wave speeds, and interior structure inference.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Primary Waves (P-Waves) > p. 60
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Why Do P-Waves Travel Faster Than S-Waves? > p. 61
S-waves are shear (transverse) waves that arrive after P-waves and may be absent at certain distances (shadow zones).
Useful for questions on wave transmission, shadow zones, and what seismic records reveal about Earth's internal state (e.g., liquid outer core blocking S-waves). Helps answer mapping of seismic wave absence and travel-path reasoning.
- FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 2: The Origin and Evolution of the Earth > Emergence of Shadow Zone > p. 20
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Secondary Waves (S-Waves) > p. 62
P-waves involve particle motion parallel to propagation, producing compression and rarefaction along the travel direction.
High-yield for seismic wave classification questions; explains arrival order on seismographs and why P-waves penetrate all media. Connects to topics on wave types, material response (compressibility), and interior Earth studies; enables answering comparative and causal questions about wave speed and transmission.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Primary Waves (P-Waves) > p. 60
- FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 2: The Origin and Evolution of the Earth > Propagation of Earthquake Waves > p. 20
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Why Do P-Waves Travel Faster Than S-Waves? > p. 61
S-waves involve particle motion perpendicular to propagation, producing shear deformation (troughs and crests).
Essential for contrasting with P-waves in exam questions; explains why S-waves cannot travel through fluids, contributes to understanding shadow zones and destructiveness. Links to material rigidity and seismic interpretation tasks.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Secondary Waves (S-Waves) > p. 62
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Why Do P-Waves Travel Faster Than S-Waves? > p. 61
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Secondary Waves (S-Waves) > p. 63
Body waves (P and S) travel through Earth's interior, while surface waves travel along the surface and cause greater damage.
Crucial for questions on seismic records, damage patterns, and probing Earth's interior; helps explain seismograph sectioning, arrival patterns, and why surface waves are most destructive. Enables reasoning on depth-related wave effects and hazard assessment.
- FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 2: The Origin and Evolution of the Earth > Earthquake Waves > p. 19
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Secondary Waves (S-Waves) > p. 63
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 5: Earths Magnetic Field (Geomagnetic Field) > Shadow Zone For Both P Wave and S Wave > p. 64
Distinguishes particle motion: transverse (perpendicular) for S-waves versus longitudinal (parallel) for P-waves.
High-yield for earthquake physics questions; helps answer questions about wave behavior, detection order, and effects on materials. Connects to topics on wave propagation, seismogram interpretation, and material response to stress.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Secondary Waves (S-Waves) > p. 62
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Why Do P-Waves Travel Faster Than S-Waves? > p. 61
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 4: Earths Interior > Primary Waves (P-Waves) > p. 60
The 'Shadow Zone' angles are the next logical target. Remember: The S-wave shadow zone (beyond 105Β°) is much larger than the P-wave shadow zone (band between 105Β° and 145Β°). Also, P-waves 'refract' (bend) at the core-mantle boundary, while S-waves are completely stopped.
Use the 'Name Mnemonic' Hack: 'P' stands for Primary (First arrival) and Pressure (Compressional/Longitudinal like sound). 'S' stands for Secondary (Second arrival) and Shear (Transverse/cutting movement). This linguistic link validates both statements without needing deep physics.
Mains GS-3 (Disaster Management): Understanding P vs S waves is the basis of 'Earthquake Early Warning Systems' (EEWS). Sensors detect the faster, non-destructive P-waves to trigger alarms/shut gas lines seconds before the destructive S-waves and Surface waves arrive.