Topics
Earth Movements
Weathering and Mass Wasting
Agents of Erosion
Climatic Regions
- Climatic Regions
- Classification of Climate and Identifying Climatic Regions (Natural Regions)
- Low-latitude Regions
- Equatorial Rainforests
- Tropical Monsoon Climate
- Tropical Savannah Type of Climate
- Tropical Deserts or Arid Type of Climate
- Mid-latitude Regions
- Mediterranean Climate
- China Type Climate or Humid Sub Tropical Climate
- Marine West European Type Climate
- High Latitudinal Regions
- Taiga or Sub-Arctic
- Tundra Climate
- Ice Sheet
- High-altitude Regions
- Highland or Mountain Type
Global Climate Change
Ocean Resources
Indian Ocean - Relief and Strategic Importance
- Indian Ocean Region
- Bottom Relief of Indian Ocean
- Continental Shelf
- Mid-oceanic Ridges
- Islands of Indian Ocean
- Ocean Basins
- Deeps and Trenches
- Distribution of Temperature and Salinity in Indian Oceans
- Indian Ocean Salinity
- Ocean Currents in Indian Ocean
- Importance of the Indian Ocean
- The Importance of Indian Ocean for India
Biomes
Disaster Management
description
- Earthquake
- Shadow zone
- Causes of Earthquakes
- Earthquake Zones in India
- Why does the earth shake?
- Earthquake Waves
- Propagation of Earthquake Waves
- Emergence of Shadow Zone
- Types of Earthquakes
- Measuring Earthquakes
- Effects of Earthquake
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Related QuestionsVIEW ALL [8]
How to locate epicentre of a given earthquake?
Take the given hypothetical data in the table. The data shows the time of arrival of P-waves and S-waves at 3 seismograph stations. Assume the scale of the map as 1 cm: 18 km. See figure.
Recording Station | P-wave arrival time ( IST) | S-wave arrival time |
Jalana | 11: 06: 06 | 11: 06: 19 |
Washim | 11: 06: 46 | 11: 07: 03 |
Aurangabad | 11: 07: 06 | 11: 07: 24 |
Procedure :
- Compute the time difference between the arrival of P-waves and S-waves for each station; this is called time lag. (It shows the distance of the seismograph from the focus. Thumb rule: For every second of time lag, the earthquake is approximately 8 km away.)
- Using the rule above, convert the time lag into the distance (seconds of time lag × 8) for each station.
- Convert this distance into centimetres as per the scale of the map.
- On a map, locate the seismograph stations.
- Draw circles, taking the seismograph stations as the centre, with the radius equal to the distance you have calculated in the previous step.
- These arcs of circles will intersect one another at a point. This point is the location of the epicentre.
In normal practice, an epicentre is located using computer models. The procedure outlined here is a much simplified version of what is normally done, although the principle is the same.
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