🗊 «Tsunami» Olena Chornobaeva Form 11

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Слайд 1


«Tsunami» Olena Chornobaeva Form 11
Описание слайда:
«Tsunami» Olena Chornobaeva Form 11

Слайд 2


Tsunami - long waves generated by the powerful influence of the whole mass of water in the ocean or other body of water.
Описание слайда:
Tsunami - long waves generated by the powerful influence of the whole mass of water in the ocean or other body of water.

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The reason most tsunamis are underwater earthquakes, during which there is an abrupt shift (raising or lowering) of the area of the seabed. The reason most tsunamis are underwater earthquakes, during which there is an abrupt shift (raising or lowering) of the area of the seabed.
Описание слайда:
The reason most tsunamis are underwater earthquakes, during which there is an abrupt shift (raising or lowering) of the area of the seabed. The reason most tsunamis are underwater earthquakes, during which there is an abrupt shift (raising or lowering) of the area of the seabed.

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The tsunami generated by an earthquake of any force, but large forces reach those that arise due to strong earthquakes. The tsunami generated by an earthquake of any force, but large forces reach those that arise due to strong earthquakes.
Описание слайда:
The tsunami generated by an earthquake of any force, but large forces reach those that arise due to strong earthquakes. The tsunami generated by an earthquake of any force, but large forces reach those that arise due to strong earthquakes.

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Earthquakes, volcanic eruptions and other underwater explosions, glaciers, meteorites and other damage above or below the water - all this has the potential to cause a tsunami. Earthquakes, volcanic eruptions and other underwater explosions, glaciers, meteorites and other damage above or below the water - all this has the potential to cause a tsunami.
Описание слайда:
Earthquakes, volcanic eruptions and other underwater explosions, glaciers, meteorites and other damage above or below the water - all this has the potential to cause a tsunami. Earthquakes, volcanic eruptions and other underwater explosions, glaciers, meteorites and other damage above or below the water - all this has the potential to cause a tsunami.

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Symptoms of tsunami
Описание слайда:
Symptoms of tsunami

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Sudden rapid withdrawal of water from the coast for a considerable distance and drying bed. The farther the sea receded, the above can be a tsunami wave. People on the beach and do not know about the danger may remain out of curiosity or to collect fish and seashells. In this case, as soon as possible to leave the coast and away from it at the maximum distance. Sudden rapid withdrawal of water from the coast for a considerable distance and drying bed. The farther the sea receded, the above can be a tsunami wave. People on the beach and do not know about the danger may remain out of curiosity or to collect fish and seashells. In this case, as soon as possible to leave the coast and away from it at the maximum distance.
Описание слайда:
Sudden rapid withdrawal of water from the coast for a considerable distance and drying bed. The farther the sea receded, the above can be a tsunami wave. People on the beach and do not know about the danger may remain out of curiosity or to collect fish and seashells. In this case, as soon as possible to leave the coast and away from it at the maximum distance. Sudden rapid withdrawal of water from the coast for a considerable distance and drying bed. The farther the sea receded, the above can be a tsunami wave. People on the beach and do not know about the danger may remain out of curiosity or to collect fish and seashells. In this case, as soon as possible to leave the coast and away from it at the maximum distance.

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Earthquake. The epicenter was located, as a rule, in the ocean. On the bank of the earthquake is usually much weaker, and it is often not at all. Earthquake. The epicenter was located, as a rule, in the ocean. On the bank of the earthquake is usually much weaker, and it is often not at all.
Описание слайда:
Earthquake. The epicenter was located, as a rule, in the ocean. On the bank of the earthquake is usually much weaker, and it is often not at all. Earthquake. The epicenter was located, as a rule, in the ocean. On the bank of the earthquake is usually much weaker, and it is often not at all.

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Unusual drift ice and other floating objects, cracking in the fast ice. Unusual drift ice and other floating objects, cracking in the fast ice.
Описание слайда:
Unusual drift ice and other floating objects, cracking in the fast ice. Unusual drift ice and other floating objects, cracking in the fast ice.

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Huge reverse faults at the edges of fast ice and reef education crowding and flow. Huge reverse faults at the edges of fast ice and reef education crowding and flow.
Описание слайда:
Huge reverse faults at the edges of fast ice and reef education crowding and flow. Huge reverse faults at the edges of fast ice and reef education crowding and flow.

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