Earthquake zones on a physical map. Earth - chronicles of life - feedback. Seismic map of Russia

As earthquake statistics show, seismological disasters account for 13% of total natural . Over the past hundred years, about 2,000 aftershocks with a magnitude of 7 or more have occurred in the world. Of these, 65 cases exceeded the 8 mark.

The situation in the world

If you look at the world map, on which seismological activity is displayed with dots, you can notice one pattern. These are some characteristic lines along which tremors are intensely recorded. The tectonic boundaries of the earth's crust are located in these zones. As statistics have established, strong catastrophic earthquakes, entailing the most devastating consequences, occur due to stress in the focus of "grinding" of tectonic plates.

Earthquake statistics for 100 years show that only on continental tectonic plates (not oceanic) about a hundred seismic catastrophes occurred, in which 1.4 million people died. In total, 130 strong earthquakes were recorded during this period.

The table shows the largest known seismic catastrophes since the 16th century:

Year Location of the incident Destruction and casualties
1556 China830 thousand people became victims. According to current estimates, the earthquake can be assigned the highest score - 12 points.
1755 Lisbon (Portugal)The city was completely destroyed, 100 thousand inhabitants died
1906 San Francisco (USA)Most of the city was destroyed, 1,500 people became victims (7.8 points)
1908 Messina (Italy)The destruction claimed 87 thousand people. human lives(magnitude 7.5)
1948 Ashgabat (Turkmenistan)175 thousand people died
1960 ChileThe largest earthquake recorded in the last century. He was rated 9.5 points. Three cities were destroyed. About 10 thousand inhabitants became victims
1976 Tien Shan (China)Magnitude 8.2. 242 thousand people died
1988 ArmeniaSeveral cities and towns were destroyed. More than 25 thousand victims recorded (7.3 points)
1990 IranAbout 50 thousand inhabitants died (magnitude 7.4)
2004 Indian OceanThe epicenter of the earthquake 9.3 points was at the bottom of the ocean, formed claimed the lives of 250 thousand inhabitants
2011 JapanAn earthquake with a magnitude of 9.1 caused the death of more than 15 thousand people and caused enormous economic and environmental impact not only for Japan, but for the whole world.

Over 30 years of the end of the 20th century, about 1 million people died in seismic catastrophes. This is about 33 thousand per year. Over the past 10 years, earthquake statistics show an increase in the average annual figure to 45 thousand victims.
Hundreds of imperceptible oscillations of the earth's surface occur every day on the planet. This is not always associated with the movement of the earth's crust. Human actions: construction, mining, blasting - they all entail fluctuations recorded by modern seismographs every second. However, since 2009, the USGS Geological Survey, which collects data on earthquake statistics in the world, has ceased to take into account shocks below 4.5.

Crete

The island is located in a tectonic fault zone, so increased seismological activity there is a frequent phenomenon. Earthquakes in Crete, according to statistics, do not exceed 5 points. With such power, there are no devastating consequences, and locals and do not pay any attention to this shaking. On the graph, you can see the number of registered seismic shocks by month with a magnitude above 1 point. You can see what last years their intensity increased somewhat.

Earthquakes in Italy

The country is located in a zone of seismic activity on the territory of the same tectonic fault as Greece. Earthquake statistics in Italy over the past 5 years show an increase in the number of monthly shocks from 700 to 2000. In August 2016, a strong earthquake of magnitude 6.2 occurred. That day claimed the lives of 295 people, more than 400 were injured.

In January 2017, another earthquake of magnitude less than 6 took place in Italy, and there were almost no victims of the destruction. However, a push has caused in the province of Pescara. The hotel Rigopiano was buried under it, killing 30 people.

There are resources where earthquake statistics are displayed online. For example, the organization IRIS (USA), engaged in the collection, systematization, study and distribution of seismological data, presents a monitor of this type:
Information is available on the site that displays the presence of earthquakes on the planet in this moment. Here their magnitude is shown, there is information for yesterday, as well as events 2 weeks or 5 years ago. You can consider in more detail the parts of the planet of interest by selecting the appropriate map from the list.

The situation in Russia


According to the statistics of earthquakes in Russia and the OSR (General Seismic Zoning) map, more than 26% of the area in the country is located in seismically hazardous zones. There may be shocks from 7 points. This includes Kamchatka, the Baikal region, the Kuriles, Altai, North Caucasus and Sayans. There are about 3,000 villages, about 100 thermal power plants and hydroelectric power stations, 5 nuclear power plants and enterprises of increased environmental danger.


Krasnodar region

Irkutsk

Due to its location near the Baikal Rift, Irkutsk's earthquake statistics record up to 40 minor shocks every month. In August 2008, seismic activity with a magnitude of 6.2 was recorded. The epicenter was in Lake Baikal, where the indicator reached 7 points. Some buildings cracked, but no significant damage or casualties were recorded. In February 2016, another earthquake of magnitude 5.5 occurred.

Ekaterinburg

Even though the growth Ural mountains has long ceased, the statistics of earthquakes in Yekaterinburg continues to be replenished with new data. In 2015, a 4.2 magnitude shock was recorded there, no one was injured.

Conclusion

Between the end of 2008 and 2011, there was a decrease in seismic activity on the planet, to a level of less than 2,500 cases per month and a magnitude above 4.5. However, after the earthquake in Japan in 2011, in the period from 2011 to 2016, there is a tendency to increase the activity of tremors around the world by almost 2 times. Earthquake statistics for recent years are as follows:

Predicting earthquakes is very difficult. Often you can say with certainty where it will happen, but when exactly it will happen is impossible to determine. However, there are biological precursors. On the eve of a strong earthquake, other representatives of the fauna living in this area begin to behave abnormally.



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The destructive power of an earthquake depends on its magnitude (in the hypocenter, i.e. in the source), the depth of the earthquake source and the distance from the epicenter (the projection point of the source on the earth's surface).

Examples of media reports and explanations of terms:
"According to ***, there, at so much Moscow time, an earthquake occurred magnitude in the source M=4.3 points on the nine-point Richter scale, at a depth of 15 km from sea level.
The epicenter of the earthquake was located 100 kilometers southeast of the city ***. Tremors were felt in the village *** force up to four points, and in the city of *** - three points (on a 12-point scale). According to the latest data, there are no casualties and serious damage. During the week, 4 earthquakes with a magnitude of 2.3 to 4.3 on the Richter scale were recorded in this area, which were also felt in neighboring regions. According to statistics provided by seismologists, the average interval between series of earthquakes of magnitude up to four points in this area is approximately *** years.

Or
"An earthquake with a magnitude, in the source, 4.3 happened there. Its epicenter was one hundred kilometers southeast of the city ***. The depth of the focus was 15 km" from sea level.

Or
A four-point earth happened somewhere today.

Magnitude earthquake (not to be confused with "strength", and leave points alone) - quantitatively characterizes its energy, at the source, on a nine-point Richter scale (0-9). Calculated based on the results of measurements by instruments (seismographs) at the closest seismic stations to the epicenter different countries. An earthquake of magnitude 6 or more, with a nearby epicenter and a shallow source, is considered strong and can cause significant damage and casualties among the population, especially if buildings and residential structures are not designed for proper seismic resistance or are built by low-skilled guest workers, with rude violations of building codes and regulations.

Force earthquake shocks (intensity) - a qualitative (felt, visible) characteristic of the degree of destruction and other manifestations on earth's surface, at a specific point on the surface of the earth. For this, a twelve-point scale (1-12) or a modified Mercalli scale is used. They differ little. The real danger is tremors with a force of four points or more.

Forecast. Before a strong earthquake, in a few minutes or even hours, domestic animals and birds begin to scream and rush about, tend to run away from the house to the street, to hide. Dogs try to lead their owners, children to a safe place. Cats take away kittens. aquarium fish- worried, trying to jump out of the water of the aquarium. Rats and mice run out of the basements of houses. Wild animals, in advance - a few hours or days before the earthquake, flocks leave the dangerous area. Snakes and lizards crawl out of their holes (even in winter, and at night and in bad weather), Birds constantly scream, fly in circles for a long time and randomly. Animals and birds lose their appetite, their behavior changes greatly - they, without attacking each other, move away from danger together.

Those who were born, grew up and lived (under natural conditions) in earthquake-prone areas have the best sensitivity. The skill is retained for a long time. Their reaction is more often selective, only to close (local earthquakes) and dangerous in strength (more than two to four points).

Seismologists and volcanologists use scientific, instrumental methods of forecasting and early warning methods: constant monitoring of seismic activity with a network of sensitive sensors, regular measurements and detection of increases in the concentration of helium and radon in the surface air and at depth, etc.

The dependence of the intensity of the earth from distance to epicenter. From closely located epicenters of earthquakes of great strength (if the "seven" of magnitude or higher strikes) - very sharp shocks and shocks are felt, intense shaking, glows, sparks are visible, an underground rumble, crackling and roar of collapsing buildings and falling, broken trees is heard, there is a sharp wind amplification. At distances of hundreds of kilometers, from the epicenter, the echoes of an earthquake reach - low-frequency, relatively slow oscillations, undulating swaying of the daytime surface of the earth. The farther - the less their vertical amplitude and longer period(up to a minute or more, with a distance to the epicenter of several thousand kilometers), with the exception of anomalously intense and resonant manifestations at certain distances from the epicenter and along large, deep tectonic faults.

Influence of tidal (gravitational) effects. Seismicity increases - on the new moon and, especially, on the full moon, as well as when the Moon is in perigee (closer to the Earth). There is also a seasonal dependence: in autumn and, especially, in winter, it shakes harder and more often than in spring and summer.

Geological factor. The greatest damage from an earthquake occurs at the outcrops of rocky rocks and if they are covered with loose deposits of small thickness, which are thrown up on their base. Safer soil conditions are territories with thick strata of loose forges. rocks in which the seismic wave weakens, is extinguished until it reaches the earth's surface.

Tsunami occur when the epicenter of the earth is near sea ​​coast. Water, at the first blow, first leaves the coast, and then, accelerating, in the form of a large wave, it falls on the coast. The brightness of the glow of marine organisms also rises sharply two or three minutes before the tsunami.

The seismic activity map is updated every 20 minutes.

To take a closer look at the area and scores, click on the source of the earthquake with the cursor, you will be taken to an enlarged area of ​​the map

Automatic GEOFON Global Seismic Moniton Map

red - last 24 hours
orange - last 1-4 days
yellow - last 4-14 days

Earthquakes in the last 30 days with a magnitude of 4 or more

EMSC+Google Map

Earthquakes in the World

red - last 24 hours
orange - from 24 to 48 hours
yellow - for the last 3-17 days
purple- from 2 weeks to 5 years

Seismic of the Atlantic Ocean

Pacific Ocean. Far East. Kuriles. Fault lines of the Pacific Ridge

Russia and Central Asia

Europe

Indonesian region

EMSC

Table data for the selected period:
http://www.emsc-csem.org/index.php?page=current&sub=list

Live Earthquake Mashup

Excellent map, direct analogue of Google planet with attached KML files
http://www.oe-files.de/gmaps/eqmashup.html

Earthquakes Canada

Map of seismic activity in Canada. All earthquakes in the last 30 days.

To view the area and scores, click on the source of the earthquake with the cursor, you will be taken to the information of the map area

The updated list of earthquakes is online.

Geophysical Service RAS


Shows the last 15 earthquakes

Map of tectonic plates of the world


Scientists have compiled a map of the largest tectonic plates:

  • Australian;
  • Arabian subcontinent;
  • Antarctic;
  • African;
  • Hindustan;
  • Eurasian;
  • Nazca plate;
  • Cooker Coconut;
  • Pacific;
  • North and South American platforms;
  • Scotia plate;
  • Philippine plate.

From theory, we know that the solid shell of the earth (lithosphere) consists not only of the plates that form the relief of the surface of the planet, but also of the deep part - the mantle. Continental platforms have a thickness of 35 km (in the flat areas) to 70 km (in the zone of mountain ranges). Scientists have proven that the plate in the Himalayas has the greatest thickness. Here the thickness of the platform reaches 90 km. The thinnest lithosphere is found in the ocean zone. Its thickness does not exceed 10 km, and in some areas this figure is 5 km. Based on the information about the depth at which the epicenter of the earthquake is located and what is the speed of propagation of seismic waves, calculations are made of the thickness of the sections of the earth's crust.

Map of faults and seismically dangerous places

The map shows the places of seismically dangerous zones. The zones are highlighted in color from green to red. The closer the color is to red, the more likely strong and destructive earthquakes are. The map was created on the data of earthquakes that have occurred since 1973.
Nuclear power plants are marked on the map. Finding nuclear power plant in a seismically hazardous area increases the danger to the population.

Hazard grade. Switch on switch off

Seismic activity scale. Richter scale. Earthquake by type of activity.

Mercalli scale Richter scale Visible action

1

0 -4.3

Vibration from an earthquake is recorded only by instruments

2

Earthquake vibrations are felt when standing on stairs

3

Earthquake shocks are felt in enclosed spaces, light vibrations of objects

4

4.3-4.8

The clinking of dishes, the swaying of trees, the tremors of an earthquake are felt in parked cars.

5

The creaking of doors, the awakening of the sleeping, the transfusion of liquid from the vessels

6

4.8-6.2

During an earthquake, unsteady walking of people, damage to windows, falling pictures from the walls

7

It is difficult to stand, the tiles on the houses are crumbling, large bells are ringing from the earthquake

8

6.2-7.3

Damage to chimneys, damage to sewer networks during such an earthquake

9

General panic from the earthquake, damage to foundations

10

Most buildings damaged*, major landslides, rivers bursting their banks

11

7.3-8.9

Bent railway tracks, road damage, large cracks in the ground, falling rocks

12

Complete destruction, waves on the surface of the earth, changes in the course of rivers, poor visibility
* Specially designed buildings with earthquake protection are able to withstand shocks up to 8.5 on the Richter scale

The amount of energy released during an earthquake

The strength of the earthquake on the Richter scale The amount of energy in an earthquake (equivalent to trinitrotoluene), t
4 6
5 199
6 6270
7 199’000
8 6’270’000
9 99’000’000

Map of earthquakes in Europe for the last 24 hours

Seismic activity on the planet over the past day

Seismic activity on the planet over the past week

| >>> Seismomonitor (overlaid on the map) | >>> USGS Seismomonitor (mapped) | >>>Seismomonitor (clickable map) | >>>Seismic monitor EUROPE |

Earthquake map according to Google service

Seismic activity map online, updated every 20 minutes. In addition, you can always find out whether there was an earthquake today or not. This allows you to more visually evaluate the information provided.

Seismic activity map of the EMSC service and Google Map

The map of seismic activity of the world allows you to select a section of the earth's surface by pressing the mouse button. In this case, the selected area will be displayed separately in the window, on which earthquake epicenters are indicated in detail. The online seismic monitor allows you to get comprehensive data when choosing any of the sources. The table shows the coordinates of the epicenters and the power of tremors, ranging from 24 hours to 30 days. Also, on the map of the region, seismic fixation stations located in the selected area are displayed.

Earthquake map from quakes.globalincidentmap.com

Earthquake map from emsc-csem.org

Behavior before, during and after an earthquake

The vast majority of earthquakes have a duration of about one, rarely more than one minute. However, the intensity of oscillations during this time is not the same. As a rule, an earthquake begins with relatively weak vibrations (sometimes imperceptible), which last 10-20 seconds, then the main phase of the earthquake occurs, at which the vibrations reach their greatest intensity, followed by a gradual decline.

Qualitatively erected and well-maintained buildings that do not have special anti-seismic measures are able to withstand earthquakes of up to six points without much damage. Buildings that are in an unsatisfactory technical condition and dilapidated, under the threat of strong earthquakes, are doubly dangerous.

Before the earthquake

Inside the house, securely attach cabinets, shelves, and furniture walls to the walls and floor. Furniture, standing and hanging objects in living quarters are placed so that if they fall, sleeping people are not injured and passages and exits from the apartment remain free. All heavy objects should be moved to the lower shelves and places. Shelves with utensils must be closed. Fix chandeliers and overhead lights securely, do not use glass lampshades.

Do not clutter up the aisles and exits from rooms and apartments with things. Flammable, caustic, poisonous liquids and powders must be securely sealed, closed in strong, fixed containers and boxes.

All family members should be well aware of the most dangerous places residential premises: in the openings of the internal main walls near these walls, at the supporting columns and under the frame beams, in the corners of the internal main walls and under solid furniture (tables, beds). And dangerous places too: near large glazed openings and partitions, corner rooms of buildings, especially the last floors.

During an earthquake

Don't panic! Quickly focus on the implementation of previously thought out actions, but be ready to act according to circumstances.

In the house/apartment:

If you are in a low, up to 2-3 floors building, then it is better to leave it quickly. This is especially true if the building is not earthquake resistant. Run out quickly, but carefully, beware of falling objects, broken wires and other sources of danger, and immediately move away from the building, away from the open area.

When on the upper floors of a multi-story building, do not rush to the stairs and elevators. Most likely, they will be overcrowded with people, and the elevators are disabled. Therefore, it is better to stay in the building and, having previously opened front door, which in the future may turn out to be jammed from distortions, quickly take the safest place in the room: under solid furniture, at the support column closest to the center of the building, in the doorway of the main walls, in the corner of the room. And always away from windows, heavy objects and equipment that could tip over. Help the disabled and the elderly.

Do not enter buildings or run around them. Once next to a tall building, stand in the doorway, this will protect you from falling pieces of glass, balconies, cornices and parapets. It's best to be on open space away from buildings and power lines.

In transport

Any transport must be calmly and quickly stopped, as far as possible from tall buildings, overpasses, bridges, power lines or anything that can collapse from strong shocks. Drivers of buses and trams, having stopped the transport, must open all the doors.

After the earthquake

While in the building, remain calm, assess the situation. Examine yourself and those around you, if necessary, provide medical care needy. Wear sturdy shoes to protect your feet from splinters and debris. Going down the stairs, check the reliability of its structures.

Check for a fire hazard. The resulting flame must be extinguished immediately. If you notice damage to the wiring, turn off the power, if it has not already been done.

According to the materials of the State Committee of the Republic of Buryatia
for civil defense and emergencies

Every day various areas of our planet are shaken by tremors. An earthquake is one of the natural disasters that cannot be prevented by man.

The only thing he can oppose to the indomitable forces of nature is the achievements of science in the field of forecasting. Systematization and monitoring of seismic activity makes it possible to avoid human casualties and destruction in time, as well as to identify areas of the greatest seismic activity.

Accounting for earthquake sources

The Earth seismic activity map is a physical map of the planet, which displays areas where earthquakes with a power of more than 4 points on the Richter scale occurred over a certain period of time. The map uses the following conventions: The diameter of the area is proportional to the strength of the tremors, and the color of the circle indicates the time interval. For example, red areas correspond to earthquakes occurring on the current date or in real time.

Seismic monitor, updated every 20 minutes


red circles - earthquakes in the last 24 hours
orange circles - earthquakes in the last 1-4 days
yellow circles - earthquakes in the last 4-14 days

EMSC and Google Map data

The map of seismic activity of the world allows you to select a section of the earth's surface by pressing the mouse button. In this case, the selected area will be displayed separately in the window, on which earthquake epicenters are indicated in detail. The online seismic monitor allows you to get comprehensive data when choosing any of the sources. The table shows the coordinates of the epicenters and the power of tremors, ranging from 24 hours to 30 days. Also, on the map of the region, seismic fixation stations located in the selected area are displayed.

List of earthquakes

To return to the beginning of the document, press Backspace or Back to the earthquake list

Seismic activity map online, updated every 20 minutes. In addition, you can always find out whether there was an earthquake today or not. This allows you to more visually evaluate the information provided.

Earthquake map according to Google service

Earth seismic activity

The images shown below are non-profit organization IRIS, founded in 1984 with the support of the National Science Foundation, is a consortium of more than 100 US universities dedicated to the study, systematization and distribution of seismological data. IRIS programs are aimed at Scientific research, education, reduction of consequences of earthquakes.

On the data below, the time is UTC (Universal Coordinated Time), to convert to Moscow, add 4 hours.

Seismic activity scale. Richter scale. Earthquake by type of activity.

Mercalli scale Richter scale Visible action

1

0 -4.3

Vibration from an earthquake is recorded only by instruments

2

Earthquake vibrations are felt when standing on stairs

3

Earthquake shocks are felt indoors, light vibrations of objects

4

4.3-4.8

The clinking of dishes, the swaying of trees, the tremors of an earthquake are felt in parked cars.

5

The creaking of doors, the awakening of the sleeping, the transfusion of liquid from the vessels

6

4.8-6.2

During an earthquake, unsteady walking of people, damage to windows, falling pictures from the walls

7

It is difficult to stand, the tiles on the houses are crumbling, large bells are ringing from the earthquake

8

6.2-7.3

Damage to chimneys, damage to sewer networks during such an earthquake

9

General panic from the earthquake, damage to foundations

10

Most buildings damaged*, major landslides, rivers bursting their banks

11

7.3-8.9

Bent railway tracks, road damage, large cracks in the ground, falling rocks

12

Complete destruction, waves on the surface of the earth, changes in the course of rivers, poor visibility
* Specially designed buildings with earthquake protection are able to withstand shocks up to 8.5 on the Richter scale

Current seismic of the Atlantic Ocean


This map shows Pacific Ocean, as well as the eastern regions of Russia - the Far East and the Kuriles. The fault line of the Pacific ridge is clearly visible.


Seismic activity in Russia and Central Asia


Map of seismic activity in Russia and Europe

Earthquakes are scary a natural phenomenon, which can bring numerous troubles. They are associated not only with destruction, due to which there may be human casualties. The catastrophic tsunami waves caused by them can lead to even more disastrous consequences.

What areas of the world are most at risk from earthquakes? To answer this question, you need to look at where the active seismic regions are. These are zones of the earth's crust, which are more mobile than the regions surrounding them. They are on the border lithospheric plates where large blocks collide or move apart It is the movements of powerful rock layers that cause earthquakes.

Dangerous areas of the world

On the globe several belts are distinguished, which are characterized by a high frequency of underground shocks. These are seismically dangerous areas.

The first of them is called the Pacific Rim, since it occupies almost the entire coast of the ocean. Not only earthquakes are frequent here, but also volcanic eruptions, so the name "volcanic" or "fiery" ring is often used. The activity of the earth's crust here is determined by modern mountain-building processes.

The second large seismic belt stretches along the high young ones from the Alps and other mountains of Southern Europe to the Sunda Islands through Asia Minor, the Caucasus, the mountains of Central and Central Asia and the Himalayas. There is also a collision of lithospheric plates, which causes frequent earthquakes.

The third belt stretches across the entire Atlantic Ocean. This is the Mid-Atlantic Ridge, which is the result of the expansion of the earth's crust. Iceland, known primarily for its volcanoes, also belongs to this belt. But earthquakes here are by no means rare.

Seismically active regions of Russia

Earthquakes also occur in our country. Seismically active regions of Russia are the Caucasus, Altai, mountains Eastern Siberia And Far East, Commander and Kuril Islands, about. Sakhalin. Earth tremors of great strength can occur here.

One can recall the Sakhalin earthquake of 1995, when two-thirds of the population of the Neftegorsk village died under the rubble of destroyed buildings. After the rescue work, it was decided not to restore the village, but to relocate the residents to other settlements.

In 2012-2014, several earthquakes occurred in the North Caucasus. Fortunately, their centers were at great depths. There were no casualties or major damage.

Seismic map of Russia

The map shows that the most seismically dangerous areas lie in the south and east of the country. At the same time, the eastern parts are relatively poorly populated. But in the south, earthquakes pose a much greater danger to people, since the population density is higher here.

Irkutsk, Khabarovsk and some others big cities are in the danger zone. These are active seismic regions.

Anthropogenic earthquakes

Seismically active occupy approximately 20% of the country's territory. But this does not mean that the rest of the world is completely insured against earthquakes. Shocks with a force of 3-4 points are noted even far from the boundaries of the lithospheric plates, in the center of the platform areas.

At the same time, with the development of the economy, the possibility of anthropogenic earthquakes increases. They are most often caused by the fact that the roof of underground voids collapses. Because of this Earth's crust as if shaken, almost like a real earthquake. And there are more and more voids and cavities underground, because a person for his needs extracts oil from the bowels and natural gas, pumps out water, builds mines for the extraction of solid minerals ... And underground nuclear explosions generally comparable to natural earthquakes in their strength.

The collapse of rock layers in itself can pose a danger to people. After all, in many areas, voids are formed right under settlements. The latest events in Solikamsk only confirmed this. But even a weak earthquake can lead to terrible consequences, because as a result of it, structures that are in disrepair, dilapidated housing in which people continue to live can collapse ... Also, a violation of the integrity of rock layers threatens the mines themselves, where collapses can occur.

What to do?

People still cannot prevent such a formidable phenomenon as an earthquake. And even to accurately predict when and where it will happen, they also did not learn. So, you need to know how you can protect yourself and loved ones during tremors.

People living in such dangerous areas should always have an earthquake contingency plan. Since the elements can catch family members in different places, there must be an agreement on a meeting place after the quake stops. The dwelling should be as safe as possible from the fall of heavy objects, furniture is best attached to the walls and floor. All residents should know where they can urgently turn off gas, electricity, water to avoid fires, explosions and electric shocks. Stairs and passages should not be cluttered with things. Documents and some set of products and essentials should always be at hand.

Starting from kindergartens and schools, the population must be taught the correct behavior when natural disaster which will increase the chances of survival.

Seismically active regions of Russia place special demands on both industrial and civil construction. Earthquake-resistant buildings are harder and more expensive to build, but the cost of building them is nothing compared to the lives saved. After all, not only those who are in such a building will be safe, but also those who are nearby. There will be no destruction and blockages - there will be no victims.

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