Press "Enter" to skip to content

Start Searching the Answers

The Internet has many places to ask questions about anything imaginable and find past answers on almost everything.

What causes the Assam earthquake 1950?

What causes the Assam earthquake 1950?

The earthquake occurred in the rugged mountainous areas between the Himalayas and the Hengduan Mountains. The earthquake was located just south of the McMahon Line between India and Tibet, and had devastating effects in both regions. Instead, this quake was caused by two continental plates colliding.

What is the Richter scale of 1950 earthquake in Assam?

The 6th biggest earthquake of the 20th century was the 1950 Assam–Tibet earthquake, also known as the Assam earthquake. It occurred on 15 August 1950 evening at 7:39 pm and had a magnitude of 8.6 on the Richter scale.

Where was the earthquake in India in 1950?

This area, south of the McMahon Line and now known as Arunachal Pradesh, is today disputed between China and India. Occurring on a Tuesday evening at 7:39 pm Indian Standard Time, the earthquake was destructive in both Assam (India) and Tibet (China), and approximately 4,800 people were killed.

Where did the earthquakes in Australia and India come from?

Scientists found it strange that the earthquakes didn’t originate from two tectonic plates rubbing against each other but from the middle of one plate. This wasn’t a complete surprise though as the the India-Australia-Capricorn plate doesn’t always work as one cohesive unit.

What was the impact of the Indian Plate on Asia?

India collided with Asia about 40-50 million years ago causing rapid uplift of the Himalayas (the Indian plate and the Eurasian plate were close to the equator back then). It’s thought that India’s coastline was denser and more firmly attached to the seabed, which is why Asia’s softer soil was pushed up rather than the other way around.

What was the cause of the earthquake in Nepal?

Saturday’s catastrophic earthquake in Nepal occurred because of two converging tectonic plates: the India plate and the overriding Eurasia plate to the north, the U.S. Geological Survey said. Tectonic plates are the large, thin, relatively rigid plates that move relative to one another on the outer surface of the Earth.