In one of Nepal’s worst natural disasters, the Gorkha earthquake struck the Gorkha District, located west of Kathmandu, on 25 April 2015 at 06:11 UTC or 11:56 am (local time) with a magnitude of 7.8 moment magnitude (Mw). A second 7.2Mw earthquake took place on 12 May 2015.
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Jetzt kostenlos anmeldenIn one of Nepal’s worst natural disasters, the Gorkha earthquake struck the Gorkha District, located west of Kathmandu, on 25 April 2015 at 06:11 UTC or 11:56 am (local time) with a magnitude of 7.8 moment magnitude (Mw). A second 7.2Mw earthquake took place on 12 May 2015.
The earthquake’s epicenter was located 77km northwest of Kathmandu, and its focus was approximately 15km underground. Several aftershocks occurred the day after the main earthquake. The earthquake was also felt in the central and eastern parts of Nepal, in areas around the Ganges River in northern parts of India, in the northwest of Bangladesh, in southern areas of the Plateau of Tibet, and in western Bhutan.
Check out our explanation on Earthquakes to understand how and why they occur!
The Gorkha earthquake was caused by the convergent plate margin between the Eurasian and the Indian tectonic plates. Nepal is located on top of the plate margin, making it prone to earthquakes. The geological structure of the valleys in Nepal (where the sediment is soft due to previous lakes) also increases the risk of earthquakes and amplifies seismic waves (which makes the impact of earthquakes more significant).
Nepal is at a high risk of natural disasters, including earthquakes. But why?
Nepal is one of the least developed countries globally and has one of the lowest standards of living. This makes the country particularly vulnerable to natural disasters. Nepal regularly experiences droughts, floods, and fires. Due to political instability and corruption, there is also a lack of governmental trust and opportunity to protect the citizens of Nepal from the impact of possible natural disasters.
At 7.8Mw, the Gorkha earthquake was devastating environmentally, socially, and economically. Let’s look at the effects of this earthquake in more detail.
A survey conducted four months after the earthquake showed that many people were suffering from depression (34%), anxiety (34%), suicidal thoughts (11%), and harmful drinking (20%). Another survey that involved 500 survivors in Bhaktapur revealed that almost 50% had symptoms of psychiatric illness.
Despite Nepal’s high risk of experiencing natural disasters, the country’s mitigation strategies before the Gorkha earthquake were limited. But thankfully, development in post-disaster relief did play a part in reducing the impact of the earthquake. For example, the 1988 Udayapur earthquake (in Nepal) led to improvements in disaster risk mitigation. Let’s take a look at some of these mitigation strategies.
Overall, Nepal’s approach to mitigation strategies needs to improve by relying less on short-term aid and providing more education on earthquake safety.
The Gorkha earthquake was caused by the convergent plate margin between the Eurasian and the Indian tectonic plates.
The environmental impacts of the Gorkha earthquake included the loss of forest and farmland (destroyed by landslides and avalanches) and changes to and contamination of water sources.
The social impacts of the Gorkha earthquake included the loss of approximately 9000 lives, nearly 22,000 injuries, and an increase in mental health problems.
Economically, £5 billion was lost due to damage to housing and significant negative effects on livelihood, health, education, and the environment.
Nepal is located on top of the plate boundary, making it prone to earthquakes. Nepal is also one of the least developed countries globally, with one of the lowest standards of living. This makes the country especially vulnerable to risks of natural disasters.
New prevention strategies as a response to the Gorkha earthquake include rebuilding buildings and systems that reduce the possible damage from future earthquakes. Organizations are also working on protecting open spaces used for relief aid.
The Gorkha earthquake was caused by the convergent plate margin between the Eurasian and the Indian tectonic plates. Nepal is located on top of the plate margin, making it prone to earthquakes. The collision between the two plates causes pressure to build up, which is eventually released.
The Gorkha, Nepal, earthquake happened on 25 April 25 at 11:56am (local time). A second earthquake took place on 12 May 2015.
The Gorkha earthquake had a magnitude of 7.8Mw according to the moment magnitude scale. A moment magnitude scale is used instead of the Richter scale, as the Richter scale is outdated. An aftershock of 7.2Mw also occurred.
The Gorkha earthquake occurred due to the convergent plate margin between the Eurasian and the Indian tectonic plates. Nepal is located on top of the plate margin, making it prone to earthquakes. The collision between the two plates causes pressure to build up, which is eventually released.
The Gorkha earthquake lasted about 50 seconds.
When did the Gorkha earthquake occur?
The Gorkha earthquake occurred on 25 April 2015 at 11:56am (local time).
Which areas were affected by the Gorkha earthquake?
The area most affected by the Gorkha earthquake was the Gorkha District, west of Kathmandu in Nepal. The earthquake was also felt in the central and eastern parts of Nepal, in areas around the Ganges River in northern parts of India, in the northwest of Bangladesh, in southern areas of the Plateau of Tibet, and in western Bhutan.
What was the magnitude of the Gorkha earthquake?
The Gorkha earthquake was 7.8Mw.
Where was the epicentre of the Gorkha earthquake?
The epicentre of the Gorkha earthquake was located 77km northwest of Kathmandu.
How deep was the focus of the Gorkha earthquake?
The focus of the Gorkha earthquake was approximately 15km underground.
What caused the Gorkha earthquake?
The Gorkha earthquake was caused due to the convergent plate margin between the Eurasian and the Indian tectonic plates. Nepal is located on top of the plate margin, making it prone to earthquakes. The collision between the two plates causes pressure to build up, which is eventually released.
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