Whereas the magnitude would sometimes be anticipated to trigger gentle harm to buildings and different constructions, specialists say proximity to fault traces, the self-love of the quake and insufficient infrastructure that can’t stand up to earthquakes all contributed to the harm.
Right here’s a more in-depth take a look at the earthquake and a few the reason why it precipitated a lot devastation:
WAS MONDAY’S EARTHQUAKE CONSIDERED “STRONG”?
The U.S. Geological Survey mentioned the quake late Monday afternoon measured 5.6 magnitude and struck at a depth of 10 kilometers (6.2 miles).
Quakes of this dimension normally don’t trigger widespread harm to well-built infrastructure. However the company factors out, “There is not one magnitude above which damage will occur. It depends on other variables, such as the distance from the earthquake, what type of soil you are on, building construction” and different components.
Dozens of buildings had been broken in Indonesia, together with Islamic boarding faculties, a hospital and different public amenities. Additionally broken had been roads and bridges, and elements of the area skilled energy blackouts.
SO WHY DID THE QUAKE CAUSE SO MUCH DAMAGE?
Specialists mentioned proximity to fault traces, the depth of the temblor and buildings not being constructed utilizing earthquake-proof strategies had been components within the devastation.
“Even though the earthquake was medium-sized, it (was) close to the surface … and located inland, close to where people live,” mentioned Gayatri Marliyani, an assistant geology professor at Universitas Gadjah Mada, in Yogyakarta, Indonesia. “The energy was still large enough to cause significant shaking that led to damage.”
The worst-affected space is near a number of identified faults, mentioned Marliyani.
A fault is a spot with a protracted break within the rock that types the floor of the earth. When an earthquake happens on one in all these faults, the rock on one aspect of the fault slips with respect to the opposite.
“The area probably has the most inland faults compared to the other parts of Java,” mentioned Marliyani.
She added that whereas some well-known faults are within the space, there are a lot of different energetic faults that aren’t properly studied.
Many buildings within the area are additionally not constructed with quake-proof designs, which additional contributed to the harm, mentioned Danny Hilman Natawidjaja, an earthquake geology professional on the Indonesian Institute of Sciences Geotechnology Analysis Heart.
“This makes a quake of this size and depth even more destructive,” he mentioned.
DOES INDONESIA USUALLY HAVE EARTHQUAKES LIKE THIS?
The nation of greater than 270 million individuals is steadily struck by earthquakes, volcanic eruptions and tsunamis due to its location on the arc of volcanoes and fault traces within the Pacific Basin often known as the “Ring of Fire.” The world spans some 40,000 kilometers (25,000 miles) and is the place a majority of the world’s earthquakes happen.
A lot of Indonesia’s earthquakes are minor and trigger little to no harm. However there have additionally been lethal earthquakes.
In February, a magnitude 6.2 earthquake killed a minimum of 25 individuals and injured greater than 460 in West Sumatra province. In January 2021, a magnitude 6.2 earthquake killed greater than 100 individuals and injured almost 6,500 in West Sulawesi province.
A strong Indian Ocean quake and tsunami in 2004 killed 230,000 individuals in a dozen nations, most of them in Indonesia.
The Related Press Well being and Science Division receives help from the Howard Hughes Medical Institute’s Division of Science Training. The AP is solely liable for all content material.