Afghanistan earthquake shakes north India, aftershocks unlikely

Subject: Geography

Section: Physical Geography (Geomorphology)

Concept:

Tremors lasting several seconds were felt in Delhi and other parts of North India as a strong 6.6-magnitude earthquake struck Afghanistan recently.

Afghanistan Earthquake

The earthquake was deep (origin 187.6 km below the earth’s surface) and the epicentre of the earthquake was in northeastern Afghanistan (earthquake prone Hindu Kush region), close to Tajikistan borders.
- Shallow earthquakes are generally more devastating because they carry greater energy when they emerge on the surface.
- Deeper earthquakes lose much of their energy by the time they come to the surface – cause less damage and are more unlikely to be followed by
- However, they spread farther as the seismic waves move radially upwards to the surface.
That is why the tremors were experienced in Punjab, Rajasthan’s Jaipur, and J&K, however, no damage is reported in India.
This earthquake was of 5-magnitude.
- Magnitude is a measure of how big the waves are, while the strength refers to the energy it carries.
Magnitude 6 earthquakes have 10 times higher amplitude than magnitude 5 earthquakes. The energy differential is even higher, 32 times for every change of 1 in magnitude.

About Earthquake

An earthquake is an intense shaking of the ground caused by movement under the earth’s surface.
The location below the earth’s surface where the earthquake starts is called the
The location directly above the hypocentre on the surface of the earth is called the
It happens when two blocks (tectonic plates) of the earth suddenly slip past one another releasing stored-up ‘elastic strain’ energy in the form of seismic waves.
These spread through the earth and cause the shaking of the ground.
They are measured on scales called the –
- Moment Magnitude Scale (Mw), based on the total moment (a product of the distance a fault moved and the force required to move it) release of the earthquake.
- The Richter scale (magnitude scale) – energy released – 0-10.
- The intensity scale/Mercalli scale – visible damage – 1-12.
Earthquakes continue to remain the most common natural hazard that cannot be predicted as no early warning systems can be developed.

Earthquake High Risk Zones in India

Western Himalayas continue to be one of the most dangerous seismic zones in the world.
According to the scientists, the Himalayan region – the 2500-km stretch from the Hindu Kush mountains to the end of Arunachal Pradesh – is due for a big earthquake (magnitude of over 8 on Richter scale) anytime.
This is because of the huge amount of energy stored along the fault lines due to the continuous interaction of different tectonic plates.
This energy can be released only in the form of massive earthquakes.

For further notes on Earthquake, refer – https://optimizeias.com/earthquake-3/