# Q2A · Discuss in detail with neat sketch any 3 types of seismic waves. Also explain the con…

Subject: Disaster Management

Exam: TEE

Reader: https://deep-learning-study-room.vercel.app/dm/#tee/papers/paper-2026-02-12/q2a

Canonical: https://deep-learning-study-room.vercel.app/read/dm/tee/papers/paper-2026-02-12--q2a/

Actual TEE paper · 100 marks · 3 hours · Q1 + any four of Q2–Q7

### Q2A. Discuss in detail with neat sketch any 3 types of seismic waves. Also explain the concept of cordon-off zone and draft typical cordon-off zone for each type of seismic waves. [10 marks]

#### Answer

**Definition.** Seismic waves are disturbances carrying earthquake energy. Body waves travel through the Earth; surface waves propagate along its surface.

Swipe across the diagram to read its labels ↔

![Seismic waves: compare particle motion](https://deep-learning-study-room.vercel.app/dm/fig/waves.3b808bf75c.svg)

Diagram: Seismic waves: compare particle motion. Labels: Seismic waves: compare particle motion | Seismic waves: compare particle motion | P wave · body wave | Push and pull parallel to travel: alternating compression and expansion. | S wave · body wave | Shearing motion perpendicular to the direction of wave travel. | Love wave · surface wave | Horizontal side-to-side shear, shown here from above. | Rayleigh wave · surface wave | Approximately elliptical rolling motion, shown in a vertical side view. | particle | particle | particle | rolling | travel → | travel → | travel → | travel → | Particle paths illustrate local movement; the wave carries energy onward.

Compare the direction of energy travel with the local movement of ground particles.

| Wave | Particle movement | Travel / key point |
| --- | --- | --- |
| P: primary | Compression and expansion parallel to travel direction. | Fastest body wave; travels through solids and fluids. |
| S: secondary | Shearing perpendicular to travel direction. | Slower than P; cannot propagate through liquids as shear waves. |
| Love | Horizontal side-to-side surface motion. | Surface wave; produces strong lateral shaking. |
| Rayleigh | Rolling, approximately elliptical motion in a vertical plane. | Surface wave with vertical and horizontal ground movement. |

“Direction of travel” means where wave energy moves. “Particle movement” means how a small part of the ground moves locally. A particle need not travel all the way from the fault to your city. Do not list Love waves as body waves.

## How shaking is recorded

A **seismometer** senses ground movement. A **seismograph** is the sensing-and-recording system; a **seismogram** is its record. A classical instrument uses inertia: the supporting ground moves relative to a suspended mass. Modern electronic instruments record a time series. Sensor, recorder and timing reference are the three basic components.

## Why P–S arrival separation is useful

P waves arrive first because they travel faster. The P–S time gap generally increases with source distance. Records from several stations constrain earthquake location. One station alone does not uniquely locate an epicentre; real location calculations use travel-time models.

A **cordon** is a controlled boundary separating an assessed danger area from safe public access. After an earthquake it follows damage and secondary hazards, not the distance travelled by a particular wave.

Swipe across the diagram to read its labels ↔

![Earthquake damage: a hazard-based cordon](https://deep-learning-study-room.vercel.app/dm/fig/quake-cordon.33e92aab0d.svg)

Diagram: Earthquake damage: a hazard-based cordon. Labels: Earthquake damage: a hazard-based cordon | Earthquake damage: a hazard-based cordon | Restricted damage area | Unstable building / debris | Controlled entry | Authorised rescue teams; structural | assessment and safe access. | Safe assembly / coordination | Outside assessed collapse and | secondary-hazard zones. | Review aftershocks, adjacent structures, utilities and new damage. | No separate fixed-radius cordon exists for P, S or surface waves.

Use the damaged building and secondary hazards to set the boundary. This is one typical earthquake-response sketch, not a separate zone for each wave.

1. **Restrict the dangerous area.** Keep the public away from unstable buildings, falling debris, damaged utilities and possible collapse zones. Specialist assessment guides the boundary.
2. **Control rescue access.** Authorised and properly equipped teams enter through managed access points. Maintain a clear route for rescue vehicles and casualty transfer.
3. **Provide safe outer coordination.** Place assembly, information, medical support and command outside the assessed danger. Account for evacuees and keep emergency routes unobstructed.
4. **Review the boundary.** Aftershocks and further structural or utility failures can change the danger. Update cordons and communicate any movement or all-clear through responsible authorities.

The question’s request for a different cordon for each seismic wave is scientifically misleading. P, S and surface waves are forms of propagating energy; they do not define standard separate operational cordon radii. Explain this distinction, then draw the hazard-based earthquake cordon shown above.

#### Illustrative application · Reading two arrivals

A station records a P arrival before an S arrival because P waves travel faster. The growing arrival-time gap with distance can help locate the source using travel-time information. A gap alone, without an appropriate velocity model, is not a universal kilometre conversion.