🗊Andrei Dmitriev, Kurnuzov Andrew 8th grade students B

Категория: Английский язык
Нажмите для полного просмотра!
Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №1Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №2Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №3Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №4Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №5Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №6Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №7Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №8Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №9Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №10Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №11Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №12Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №13Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №14Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №15Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №16Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №17

Вы можете ознакомиться и скачать Andrei Dmitriev, Kurnuzov Andrew 8th grade students B. Презентация содержит 17 слайдов. Презентации для любого класса можно скачать бесплатно. Если материал и наш сайт презентаций Вам понравились – поделитесь им с друзьями с помощью социальных кнопок и добавьте в закладки в своем браузере.

Слайды и текст этой презентации


Слайд 1






Andrei Dmitriev, Kurnuzov Andrew 8th grade students B
Описание слайда:
Andrei Dmitriev, Kurnuzov Andrew 8th grade students B

Слайд 2


Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №2
Описание слайда:

Слайд 3





The vertical motions lead to a drastic lowering or raising of the rocks. Typically, the offset is only a few centimeters, but the energy released when moving billions of tons of rock, even a small distance is enormous.
The vertical motions lead to a drastic lowering or raising of the rocks. Typically, the offset is only a few centimeters, but the energy released when moving billions of tons of rock, even a small distance is enormous.
Описание слайда:
The vertical motions lead to a drastic lowering or raising of the rocks. Typically, the offset is only a few centimeters, but the energy released when moving billions of tons of rock, even a small distance is enormous. The vertical motions lead to a drastic lowering or raising of the rocks. Typically, the offset is only a few centimeters, but the energy released when moving billions of tons of rock, even a small distance is enormous.

Слайд 4


Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №4
Описание слайда:

Слайд 5







This sudden release of energy stored in compressed or stretched rocks.
It manifests itself in tremors and vibrations of the earth's surface.
Описание слайда:
This sudden release of energy stored in compressed or stretched rocks. It manifests itself in tremors and vibrations of the earth's surface.

Слайд 6





The second reason reflects deeper processes occurring in areas along the edges of the shifting plates, where the edges of these masses are immersed in the Earth's crust Earth's mantle at depths of about 500 km re-absorbed, absorbed. For this reason, there are already more major earthquakes 
The second reason reflects deeper processes occurring in areas along the edges of the shifting plates, where the edges of these masses are immersed in the Earth's crust Earth's mantle at depths of about 500 km re-absorbed, absorbed. For this reason, there are already more major earthquakes
Описание слайда:
The second reason reflects deeper processes occurring in areas along the edges of the shifting plates, where the edges of these masses are immersed in the Earth's crust Earth's mantle at depths of about 500 km re-absorbed, absorbed. For this reason, there are already more major earthquakes The second reason reflects deeper processes occurring in areas along the edges of the shifting plates, where the edges of these masses are immersed in the Earth's crust Earth's mantle at depths of about 500 km re-absorbed, absorbed. For this reason, there are already more major earthquakes

Слайд 7


Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №7
Описание слайда:

Слайд 8


Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №8
Описание слайда:

Слайд 9





The first seismograph, which had scientific value, was built in 1879 in Japan, Ewing. As the cargo was for a pendulum cast iron ring weighing 25 kg, suspended on steel wire.
The first seismograph, which had scientific value, was built in 1879 in Japan, Ewing. As the cargo was for a pendulum cast iron ring weighing 25 kg, suspended on steel wire.
Описание слайда:
The first seismograph, which had scientific value, was built in 1879 in Japan, Ewing. As the cargo was for a pendulum cast iron ring weighing 25 kg, suspended on steel wire. The first seismograph, which had scientific value, was built in 1879 in Japan, Ewing. As the cargo was for a pendulum cast iron ring weighing 25 kg, suspended on steel wire.

Слайд 10





Currently, inducted into the practice of monitoring large areas: near the major faults are placed devices on which information is transmitted via satellite connection to the centers, where is processed. 
Currently, inducted into the practice of monitoring large areas: near the major faults are placed devices on which information is transmitted via satellite connection to the centers, where is processed.
Описание слайда:
Currently, inducted into the practice of monitoring large areas: near the major faults are placed devices on which information is transmitted via satellite connection to the centers, where is processed. Currently, inducted into the practice of monitoring large areas: near the major faults are placed devices on which information is transmitted via satellite connection to the centers, where is processed.

Слайд 11





Другой метод основан на определении содержания воды в породах. В напряжённых породах происходит увеличение объёма пор, а тем самым и водосодержания.
Другой метод основан на определении содержания воды в породах. В напряжённых породах происходит увеличение объёма пор, а тем самым и водосодержания.
 Издавна известно, что люди использовали более чутких животных для предупреждения о возможной опасности.
Описание слайда:
Другой метод основан на определении содержания воды в породах. В напряжённых породах происходит увеличение объёма пор, а тем самым и водосодержания. Другой метод основан на определении содержания воды в породах. В напряжённых породах происходит увеличение объёма пор, а тем самым и водосодержания. Издавна известно, что люди использовали более чутких животных для предупреждения о возможной опасности.

Слайд 12






Not bad a presentiment of natural disturbances and attack pets. It is well known that dogs, chickens and pigs shortly before the onset of disasters are changing their behavior, give in to apathy and refuse to eat.
Описание слайда:
Not bad a presentiment of natural disturbances and attack pets. It is well known that dogs, chickens and pigs shortly before the onset of disasters are changing their behavior, give in to apathy and refuse to eat.

Слайд 13





. Snakes, especially poisonous, in anticipation of an approaching earthquake is a few days leave the inhabited burrows. So do lizards and ants. Some scholars are inclined to explain this undeniable fact highly sensitive to temperature changes in the skin of the soil 
. Snakes, especially poisonous, in anticipation of an approaching earthquake is a few days leave the inhabited burrows. So do lizards and ants. Some scholars are inclined to explain this undeniable fact highly sensitive to temperature changes in the skin of the soil
Описание слайда:
. Snakes, especially poisonous, in anticipation of an approaching earthquake is a few days leave the inhabited burrows. So do lizards and ants. Some scholars are inclined to explain this undeniable fact highly sensitive to temperature changes in the skin of the soil . Snakes, especially poisonous, in anticipation of an approaching earthquake is a few days leave the inhabited burrows. So do lizards and ants. Some scholars are inclined to explain this undeniable fact highly sensitive to temperature changes in the skin of the soil

Слайд 14





As part of the ESP is not inferior to reptiles and crocodiles.
As part of the ESP is not inferior to reptiles and crocodiles.
December 17, 1987 on the island of Kyushu, dozens of individuals have begun to publish an alarming growling and bending arch, perform an intricate dance.
Описание слайда:
As part of the ESP is not inferior to reptiles and crocodiles. As part of the ESP is not inferior to reptiles and crocodiles. December 17, 1987 on the island of Kyushu, dozens of individuals have begun to publish an alarming growling and bending arch, perform an intricate dance.

Слайд 15





 Scientists argue that the approach of an earthquake can prevent at least 130 animals. 
 Scientists argue that the approach of an earthquake can prevent at least 130 animals.
Описание слайда:
Scientists argue that the approach of an earthquake can prevent at least 130 animals. Scientists argue that the approach of an earthquake can prevent at least 130 animals.

Слайд 16






A new type of earthquake, Japanese scientists discovered. Earthquake, described by researchers led by Professor Ito Iosihiro have ultra-low frequency. Identified seismic processes can lead to fluctuations in the magnitude 3 to 3.5 points. However, the shocks are so slow that their man does not feel. However, these variations contribute to the growth pressures in a seismically active zones.


A new type of earthquake, Japanese scientists discovered. Earthquake, described by researchers led by Professor Ito Iosihiro have ultra-low frequency. Identified seismic processes can lead to fluctuations in the magnitude 3 to 3.5 points. However, the shocks are so slow that their man does not feel. However, these variations contribute to the growth pressures in a seismically active zones.
Описание слайда:
A new type of earthquake, Japanese scientists discovered. Earthquake, described by researchers led by Professor Ito Iosihiro have ultra-low frequency. Identified seismic processes can lead to fluctuations in the magnitude 3 to 3.5 points. However, the shocks are so slow that their man does not feel. However, these variations contribute to the growth pressures in a seismically active zones. A new type of earthquake, Japanese scientists discovered. Earthquake, described by researchers led by Professor Ito Iosihiro have ultra-low frequency. Identified seismic processes can lead to fluctuations in the magnitude 3 to 3.5 points. However, the shocks are so slow that their man does not feel. However, these variations contribute to the growth pressures in a seismically active zones.

Слайд 17


Andrei Dmitriev, Kurnuzov Andrew 8th grade students B, слайд №17
Описание слайда:



Похожие презентации
Mypresentation.ru
Загрузить презентацию