This unknown error can destroy Socal

Located below the famous beaches in California, mountains and urban areas is an evil network of earthquake errors – some of which are so bad that their names are burned in the awareness of the collective state.

Of course, there is the great San Andreas, which caused its massive earthquake in the San Francisco earthquake in 1906, which sparked the reputation of many films, video games, books, shirts and collections.

It is also known in Los Angeles Nioport-Englywood, which launched the 1933 Long Beach earthquake in the modern history of Southern California.

The big earthquake's error near the line that moved Monday morning in the mountains of San Diego County, however, is relatively mysterious. But Elsinore's mistake is part of a larger seismic zone that is afraid of experts and believes that more people should know about it.

The rift area is actually one of the largest areas in southern California, according to Caltech, but “in historical times, it was one of the most goals.”

However, lack of activity is a degraded power. Seismologist Lucy Jones, a super technology researcher, said that the error is able to generate an earthquake of 7.8.

“The Elsinore error is one of the main risks in southern California,” Jones said.

The Sonian desert ESINURE desert passes through the Empire Province via the western edge of Riverid County Communities such as Timikola, Maurita and Lasinor Lake.

By the time when it reaches Corona, it is divided into two parts – China's mistake, which is heading towards the Cheno Hills; Whiter, which is located near the outskirts of the province of Whiteer, La Habra Heights, Hasinda Heights and Roland Heights, and no Habra, Briya and Yarra Linda in Orange County.

The frightening and special probability will be an earthquake that precedes the Elsinore Northwest error on Whittier's mistake. “It would” pour all the energy directly into the Los Angeles basin, “Jones said. It is one of the frightening earthquakes. ”

According to one of the virtual scenario published by the American Geological Survey, an earthquake reached 7.8 years in the Elsinore rift area, including the Whittier error, can bring “violent” – enough to damage the buildings or even its rise, at a height, in formulation, in Ait, in Ait, in Air, Yorba Linda, Placentia, Chino Hills, Corona, Lake Elsinore, Murieta and Temecula.

This is much larger than the San Fernando Valley part, which witnessed a “violent” vibration during the 1994 Northdage earthquake, which was 6.7.

The “severe” shake – which is enough to drop the chimneys and badly damage the building – may feel badly – away from the mistake it torn, including in the center of Los Angeles, east of Los Angeles, Long Beach, Al -Hamra, West Kovina, Bomona, Ontario, Riverzid, Downey, Norwok, Santa Anna, Garden Grov, Ann Urang, Orange, Oranjin, Irvin.

The “very strong” shaking, including the San Fernando Valley, Westidaid, South Bay, Los Angeles and Long Beach ports, Orange Coast, Rancho Kokamonga, Fontana and San Bernardino.

No earthquake in the modern era was strong, or such a destroyed fundamental shake across such a wide range of California.

The last earthquake in southern California occurred 7.9 in 1857, when San Andreas was torn between the provinces of Monterrey and Los Angeles. The last equivalent in northern California was the great 1906 earthquake, which was torn by San Andreas between the provinces of Humoult and Santa Cruz and destroyed many San Francisco.

Katecar, a geologist in the American geological survey, said that Elsinor's mistake could be considered by the brother of Andreas, along with San Jacinto's big mistake. The St. Jacinto Rift area begins in the Kajon Corridor and moves southeast of San Bernardino and Riferside Province before heading to Imperial Province.

All three faults move at a relatively high rate on average- which means that, in general, they are more likely to collapse during the human life period. San Andreas and San Jacinto move at a rate of 20 millimeters on average annually, while Elsinore moves in a more modest clip of about 5 millimeters annually. On the contrary, the notorious Nioport-England error moves much slower, at a rate of 1 mm annually.

“There are some risks that these might be the following risks,” Charry said about the risk of its rift in Elsinor. “We focus a lot on San Andreas, but we have a full range of active mistakes that accumulate stress.”

The size of the two is 5.2 temblor was an unstable reminder of the error strength. While the earthquake, which was concentrated near Julian, was shaken throughout the area, there were no major injuries or damage. But this may not be the case next time, especially if the earthquake is approaching the main cities.

The two earthquake led to at least nine interests of 2.5 or more, including the size of 4 after a few more than an hour.

The 5.2 earthquake was preceded by an earthquake of 3.3, which is now a comma.

Saint Jacinto's rift area itself – it is cut directly by the heart of the inner empire, under many densely populated areas. Saint Jacinto and San Andreas's mistakes can explode together in an earthquake of 7.5.

California is considered at risk of large earthquakes because it is located on the edge of the boundaries of the Tktone plate, where the Pacific plate – on which San Diego, Los Angeles and Santa Barbara – are slowly heading in the northwest for North America, on which San Francisco, Central Valley and Lake Big Bear are located.

This strain accumulates for decades and centuries, and is eventually released in the form of earthquakes around the boundaries of the tectonic plate.

Elsinore is a very long mistake. The longer the rupture of an earthquake, the total seismic energy is produced.

“The analogy resembles a small small caso tool, you cannot make it very loud,” said Charry. “But if you get to a pipe … you can get a much higher sound because it is a larger tool, so more energy can be pumped through this system.”

Some of the largest California cities have made great steps in the request to re -adjust weak buildings in terms of seismic, but the weaknesses remain. The Times investigation, which was published in November, found that a number of southern California suburbs have no active plans to require flimsy residential buildings, known as the “soft story”, which is modified against earthquakes.

One of the dangerous places is the inner empire, where brick buildings – a serious danger that Los Angeles ordered them before fixed decades – is still a threat, despite the rift areas located below the region.

Another risk is likely to be defective solid frame buildings, which must be re -equipped in a few cities, such as Torrance, Santa Monica and West Hollywood, but not in Los Angeles.

Los Angeles and Brang provinces did not have great experience in severe destructive earthquakes during the last generation.

Since 1998, there has been only one earthquake of 5 or more under the provinces of Los Angeles and orange. This was an earthquake of 5.1 in 2014 in Brea, which caused damage to more than $ 2.5 million in that city, Volverton or Habra.

There was also a 5.4 Chino Hills earthquake in 2008. It was focused in San Bernardino Province, but East Los Angeles and Orange provinces caused slight damage.

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