Earthquakes
ICSE · Class 9 · Geography
Complete topic list for Earthquakes in ICSE Class 9 Geography. Key concepts, sub-topics, and what to focus on for board exams.
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Key Terminology – Focus, Epicentre, and Seismograph
- The FOCUS (also called the hypocentre) is the point inside the Earth's crust or mantle where the earthquake originates — where rocks first begin to fracture.
- The EPICENTRE is the point on the Earth's surface directly above the focus. The intensity of shaking is maximum at the epicentre.
- Seismic waves (shock waves) travel outward from the focus in all directions and are recorded by a Seismograph (also called Seismometer).
Causes of Earthquakes
- There are four main causes of earthquakes: (i) Volcanic Eruptions, (ii) Folding and Faulting, (iii) Plate Tectonics, and (iv) Anthropogenic (human-made) Factors.
- VOLCANIC ERUPTIONS: Gas explosions during volcanic activity trigger earthquakes. The eruption of Krakatoa (between Sumatra and Java) caused 30–40 metre high tsunamis, killing over 36,000 people. Its i
- FOLDING AND FAULTING: A fault is a fracture in rock along which observable displacement has occurred. Earthquakes along faults are called tectonic earthquakes. The San Andreas Fault in California caus
Measurement of Earthquakes – Richter Scale and Intensity
- The magnitude of an earthquake is most commonly measured by the RICHTER SCALE, devised by Charles F. Richter in 1935 and modified in 1965 by Richter and Beno Gutenberg.
- The Richter Scale is an open-ended, logarithmic scale — it has no fixed maximum or minimum.
- The scale relates to the energy released at the earthquake centre and estimates the severity.
Distribution of Earthquakes – Major Earthquake Belts
- Earthquakes follow a definite pattern of distribution worldwide. There are THREE major earthquake belts and one additional zone.
- 1. THE CIRCUM-PACIFIC BELT (Pacific Ring of Fire): The most active belt; accounts for about 66% of all earthquakes. It extends along the west coasts of North and South America, through Alaska, Japan,
- 2. THE MID-ATLANTIC BELT: Extends along mid-oceanic ridges in the Atlantic Ocean. Caused by seafloor spreading (divergent plate boundaries). Earthquakes are shallow focus (less than 70 km) and of mode
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