What is shock?

When an earthquake hits, it can get into three different classifications. Some earthquakes are regulations and are usually smaller earthquakes that occur in approximately the same area as a larger earthquake later. Others are a big event or Mainshock, which will be the earthquake of the largest size that occurs. This large earthquake may be followed by others that are smaller, but can still be dangerous, and these are called shocks. Such an earthquake occurs near the main Mainshock, as well as a harbinger, and could appear for some time after the main events of Mainshock. Within the first few days, the greatest danger of another earthquake with a relatively high size is compared to the main mainshock. This danger may exist for several reasons.

with a large main earthquake, especially in a well -planned area, structural and harm can be many different things. High -size shocks could pose a significant risk,Because it could complete the structural damage of certain things. This could cause buildings, gas lines or other serious problems. It greatly increases the chance that more people will lose their property or get hurt. The combined effect of the large Mainshock and only slightly less shock is sometimes devastating.

One thing that can confuse people is when aftershock has a higher size rating than Mainshock. In this case, the whole set of earthquakes must be that bothers an area that must be reclassified. Suddenly he is not "PO" "PO" and becomes Mainshock. Mainshock moves to the forecast state. It may take a while to look at the series of earthquakes and determine which one was central and which were front and shocks.

It was often found that recovery from shocks of any kind requires time. This is particularly true of shocks that may continue to occur many years afterto Mainshock. It has recently been proposed that the distance of the earthquake from tectonic plates can control the way the soil reacts afterwards. If the earthquake was far from tectonic plates, the amount of recovery time could take much longer. For example, some earthquakes that now occur on the US Midwest are considered to be the shakes of those that occurred in the early 19th century. The Earth seems to have a long memory in this theory.

For people who have just encountered a larger earthquake, it is necessary to consider the possibility to experience a shock. If the dwelling is dangerous, it should be ascended until it is cleaned, or if a few things seem to be wrong, it's fast cleaning. Such times can be difficult to endure and are a more terrifying potential for adding earthquakes. Like the Earth, it recovers through these continuing gloomy, many people can find themselves on recovering; Ofencshocks může být jak emocionální metafora, tak fyzický vyjádření Země.