How do we protect it

Earthquake protection

The earthquake was reported on Saturday at 9:38 AM Pacific Time 10 miles from Hollister, California, according to the U.S. Geological Survey. It measured 3.3 kilometers 13 miles from Soledad, California, 14 miles from Salinas, California, 16 miles from Pridal, California, and 23 miles from Gilroy, California.

On Friday, it measured 6.5 near the strongest earthquake in Tonoba state in over 65 years. An earthquake (also known as an earthquake, tremor, or earthquake) is the shaking of the Earth’s surface caused by the sudden release of energy into the Earth’s lithosphere, which creates seismic waves.

The earthquake causes damage

Earthquake

Earthquakes can range from those that are so weak that you don’t feel violent enough to push things and people in the air and wreak havoc across entire cities. Seismic activity or seismic activity of the region is the frequency, type, and magnitude of earthquakes that have been subjected for some time. The word jitter is also used to shake non-seismic earthquakes. In the past ten days, there have been no earthquakes of magnitude 3.0 or greater centered close. If you are inside when you feel the earth tremor, slide down to the ground.

before and after

Take a shower under a solid piece of furniture, or seek shelter. Avoid danger points near windows, hanging objects, mirrors, or long furniture. Maintain the position until the ground stops shaking, it is safe to move around, in modern homes and buildings, the entrances are no safer, and do not protect you from flying or falling. Be under a table instead. Don’t run outside. If you are outside, go outdoors, away from buildings, electricity lines and trees. Be wary of falling rocks and other debris that the earthquake can mitigate, if you’re on the beach, move to higher ground as soon as the vibration stops to avoid a potential tsunami. Check out your phone and utilities. Be aware of potential hazards, including falling utility lines, fallen objects, and damaged air vents.

The scales used to describe the magnitude of the earthquake began on the Richter scale in 1930. It is a relatively simple measure of the event’s amplitude, and its use has become minimal in the 21st century. Seismic waves travel through Earth and can be recorded by seismometers at great distances. The surface wave size was developed in the 1950’s as a way to measure remote earthquakes and improve accuracy for larger events. The torque gauge not only measures the amplitude of the shock, but also takes into account the seismic moment. The Japan Meteorological Authority’s seismic intensity scale, the Medvedev-Spoonwire-Karnick scale, and the Mercury intensity scale are dependent on the observed effects and are related to the vibration intensity.

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