What caused and why did a building for Bangkok’s collapse?

A large earthquake in Myanmar on Friday caused more than 1,000 deaths and caused the collapse of numerous structures.

Although myanmar is a high risk area for earthquakes, damage to the buildings was widespread.

On the other hand, Bangkok is not considered an earthquake-inclination. Thai Capital Friday Epicenter has dropped 1000 km (621 miles) and a half-starving building in the city.

We will explain what this earthquake is caused and so far away.

The upper layer of the earth is divided into different parts called all-moving tectonic tiles. Some together with each other, others are on top of each other.

This is the action that causes earthquakes and volcanoes.

Myanmar is considered one of the most geologically active “active” areas, because it sits on the approximation of four of these tectonic tiles – Eurasian plate, India plate, Sounda and Burma Mikroplate.

Himalayas, the Indian plate collided with the Eurasian plate, occurred by 2004 tsunami as a result of Indian plate moving under the Burma Microplat.

Dr. Rebecca Bell, the Tectonics in the Imperial College, the reader in London, allowing this action, all of the shortcomings, all of the shortcomings to place all the shortcomings, “slip” to the tectonic tiles.

Myanmar is cut off the south of north and this is a great tool called Sagaing shortcomings that are more than 500 km (746 miles).

Early information was a “strike shift” that the movement that caused the magnitude of 7.7 magnitude of Friday horizontally.

This is adapted to the action inherent in sagaing.

As the plates pass over each other, they can suddenly build friction until the place changes and the earth causes an earthquake.

Earthquakes can be up to 700 km (435 miles) from the surface. This was only 10 km from the surface, made it very shallow. This increases the amount of shaking on the surface.

The earthquake was very large – 7.7 in the moment. According to US Geological Survey, he produced more energy from the atomic bomb in Hiroshima.

The size of the earthquake was due to the type of sin, Dr. Bell said.

“Straight Nature (sin) can fall on large areas of earthquakes – and the larger the sin is the bigger the sliding earthquake,” he said.

“In the last century, 7 or more earthquakes were in this region.”

This flat sin can also lead to many energy lengths – this is 1200 km south of Thailand.

The surface is determined by the type of soil that earthquakes are felt.

In soft land – what is being built on Bangkok – seismic waves (vibrations of the earth) slow down and grow.

Thus, the geology of Bangkok would make the place more.

Dramatic images arise in high-rise buildings in Bangkok during the earthquake – Beating water from Doofop pools – Auditor-General Office seems to be the only skyscraper to crumble the unfinished headquarters for Bangkok’s Chatuhak district.

Since 2009, in Bangkok, earthquakes in the earthquakes, earthquakes in earthquakes and earthquake engineering, there was no comprehensive security standards to endure earthquakes in London.

This means that older buildings would be particularly sensitive.

It is not uncommon for the construction of earthquake-resistant buildings and unlike Thailand, as opposed to Thailand, and Thailand often does not experience earthquakes.

Dr. Emily, a professor of architectural engineering in Cambridge University, the larger buildings have been strengthened and strengthened, as in California, West Canada and New Zealand.

Again, the collapsed building was new – in fact, when the earthquake occurred – and the updated building standards were applied.

However, after investigating the video, Dr. Málaga-Chuquitaype seems to be not recommended in the “straight slab” construction process, which the “a flat slab” construction process, which is experiencing a “flat plate” construction process.

“A flat slab ‘system is the method of building the floors to rest in direct columns without using the rays,” he said.

“Imagine, just a table supported with your feet, there is no additional horizontal support.

“Although the value and architectural advantages of this design, it is weak during earthquakes, often fails in a fragile and suddenly (almost explosive).”

Mandalay in Myanmar, the land was very close to the shivering from Bangkok to much serious vibrations.

Although myanmar regularly raised earthquakes, Dr. Ian Watkinson, a teacher in the field of land sciences at Royal Holloway University, he thought that many buildings were likely to be proven to earthquake.

“In addition to the general poverty, the main political rise, other disasters, in 2004, the Indian Ocean Tsunami – the country in 2004 distracting the unexpected risks of earthquakes,” he said.

“This means that in many cases, design codes are not applied and the construction is prone to the areas of seismic risk, such as flood plains and steep slopes.”

The parts of the Mandalay and its buildings are also sleeping in the flood of the flood of Ayerwaddy River. This makes them very sensitive to a process that liquefies them.

This occurs when the soil is high water and causes the trembling sediment loss and act like liquid. It can no longer catch them because the land increases the risk of landslides and building the building.

Dr., after an earthquake due to afterhocks, he warned that near the shocks near the shocks near the shocks near the shocks near the shocks near the shocks.

“Often nobles are smaller than the main shock and tend to reduce measurement and frequency over time,” he said.

Additional report by Vicky Wong