Theories of the emergence of earthquakes
Since its inception, the earth was a hot body
like the other planets, and when
cold fact that the hydrosphere and atmosphere to attract his antenna, and with
the increasing cold .. Formed solid layer of Foreign Affairs, known as the
cortex, but the ground under a hot date, and contains magma cities of Limoges
Bz on the erosion of hard rock in the crust of solid and downloaded or shipped
Bajhadat and great potential for the very increase over time, and the crust
itself is composed of a set of sheetrock giant very , each carrying a plate of
which continent or more, and spoke process of loading or shipping primarily in
the areas of convergence of these panels with each other, the so-called
scientists faults or faults that define the ends and beginnings of plates
bearing the continents, and when more than shipping or pressure on the ability
of theserocks on the possibility not only be able to release this energy in the
form of waves suddenly a strong movement spread in all directions, penetrating
crustal rocks, and makes them vibrate and tremble, as is known, in the light of
that ..Originated on the ground a group of vulnerable areas in the earth's
crust are centers of seismic activity, or exits of breathing through which the
ground of what is going on inside of the energy concerned need to be a starting
point, and so-called "belts of earthquakes", namely: belt Pacific
extending from South-East Asia shoe Ocean Alhadeshmala, and belt western North
America, which extends along the Pacific Ocean, and a belt west of the
Americas, including Venezuela, Chile and Argentina, and a belt of central
Atlantic Ocean, including western Morocco, and extends as far north as Spain,
Italy, Yugoslavia, Greece and northern Turkey, and meet this fault when it
extends to the southeast with the "mountains of Zagros "between Iraq
and Iran, an area near the" Ring of the Himalayas. " And alpine belt,
including the Alps in the south of Europe. Belt and northern China, which runs
north China introduced from east to west, and meet with a crack of the
Caucasus, and the west Pacific Ocean with a crack. There is another belt of the
weakest earthquake belts, and extends from the southern Anatolian fault along
the Dead Sea as far south as the Gulf of Suez, South Sinai, Red Sea and then
the center of the great African Valvalq, and affects the regions of Yemen and
Ethiopia and the Great Rift Valley. The Earth and one unit, but it's hard to
volcanoes the earth's crust, and the pressures in different regions of lead to
the occurrence of seismic activity can not link between him and the seismic
activity occurs in another area, in light of that
.. Acquired all the belt
seismic nature of the particular different from the other in terms of the
nature Alaradih (geological) and subsurface structures, which can be with her
say that seismic activity is special to this area, does not mean convergence
time of occurrence of seismic activity on the belts of earthquakes of different
that there is a consensus at the time of occurrence with each other, but due to
many factors inside the ground is still under study of the man. The Earth and
one unit, but it's hard to volcanoes the earth's crust, and the pressures in
different regions of lead to the occurrence of seismic activity can not link
between him and the seismic activity occurs in another area, in light of that
.. Acquired all the belt seismic nature of the particular differ from the
others in terms of the nature of the geological and subsurface structures,
which can be with her say that seismic activity is special to this area, does
not mean convergence time of occurrence of seismic activity on the belts of
earthquakes of different that there is a consensus at the time of occurrence with
each other , but due to many factors inside the ground is still under study of
the man. earthquakes is a displacement of the layers earth Causes of earthquake
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