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The tectaunique is a field study of geology that focuses on misrepresentations of rock ensembles.
The tectaunique plates is a theory unifying the past and present history of the Earth, on a global scale, linking the deformations and movements of the earth's crust to the internal forces of the Earth: rigid plates rock slide on the mantle less viscous.

tectaunique plates

The tectaunique plates helps explain the formation and evolution of the earth's crust over geologic time.
According to this theory, continents and ocean floors are made up of plates that float on the asthenosphere.

tectaunique plates (resulting continental drift) is the current model the inner workings of the Earth.
She is the surface expression of convection taking place in the terrestrial mantle.

A vocabulary first. The tectaunique is this part of geology who studies the nature and causes deformation of rock ensembles,
more specifically in this case, deformations, large-scale, the lithosphere land.

The major risks

The tectaunique plates

The theory of tectaunique plates, appeared in the early sixties, to understand the volcanic and seismic nature of our planet.

The internal structure of the earth


The land is composed of concentric layers of nature and of different thickness. From the center outward, can be distinguished:

The lower mantle and the majority of the upper mantle form the asthenosphere.
The external part of the upper mantle and crust form the lithosphere.
Both sets are distinguished by their rigidity strong for the lithosphere, low for the asthenosphere.


The plates

The lithosphere, rigid and brittle, is fragmented into several fragments, plates.
Sept major plates cover the earth's surface. Des mouvements de convection au sein de l'asthénosphère rendent mobiles ces plaques, avec des vitesses de quelques centimètres par an. The movement of convection within the asthenosphere make mobile these plates, with speeds of a few centimetres per year.
This phenomenon, commonly known as continental drift, leads the contact zones plates of relative movements of divergence, convergence or coulissage.

The plates land

The magma is the liquid that is formed by partial melting of the Earth's mantle (or more rarely crust). This fluid, more or less rich in dissolved gases, can reach a depth temperature 1 300 ° C.

The convection in the asthenosphere is due to rise from the base of the mantle of hot materials, less dense. In going back to the surface, they cool, become more dense and replongent then to the depths to get warm again.
These eddies brew across the asthenosphere to a very low speed (1cm/year).

The divergence

The difference of two plates is the basis for the establishment of the oceanic crust.
The areas of divergence of plates are marked on the bottom of the oceans by the oceanic ridges, which are the largest volcanic system on Earth.
They correspond to mountain of magma which, when arriving at the surface hardens and then form the oceanic crust.
The newly formed crust away from sides of the ridge, and is the divergence.

The convergence

The convergence between two plates is the main cause of the formation of mountain ranges, volcanoes and earthquakes.
When two plates converge, the quantity of material that disappears under the mantle is equal to that formed at the back.

There are three types of convergence:

The Alps have themselves been trained by the collision of the African plate and the Eurasian plate.

Croute LAND

The coulissage

During the convergences and divergences, the movements are substantially perpendicular to the border plates.
When this movement is mainly parallel to the border, the phenomenon is called coulissage.
Like the convergence between two continental plates, coulissage resulting in a strong earthquake and volcanic almost non-existent.
Thus, the hole-San Andreas, which marks a coulissage between the Pacific Ocean plate and the continental plate of North America, is responsible for many earthquakes affecting the region of San Francisco.

A plaque volume is a rigid, thick low compared to its surface.

The tectaunique plates is a global unifying scientific theory proposing that the deformation of the lithosphere are connected to the internal forces of the earth and that these distortions result in the severing of the lithosphere in a number of rigid plates (14) moving in relation to each other by slipping on the asthenosphere.

The lithosphere, the outer layer of Earth is divided into rigid plates that float and move on the asthenosphere, more ductile.Early concepts, balbutiés from the eighteenth century, have been scientifically formulated in 1912 by the German Alfred Wegener climatologist from Cartographic considerations, structural, paleontological and paleoclimate.

The boundaries between each plate are where the majority of volcanoes and earthquakes. On the scale of geological time, the crust of the Earth is constantly moving. His movements incessant digging huge cracks at the bottom of oceans, continents grow and raise large mountain ranges.

The tectaunique plates

If you cut on a map of Africa, Europe and Asia, North America and South Australia, it is easy to combine into a single package. It can be seen for example that Africa fits in South America.

The west Africa and Brazil formed only a single continent.
Some old fossils 200 million years can be found on these two continents but nowhere else.

The lithospheric plates move at the Earth's surface for several hundreds of millions of years.
So far, they argue 2 to 20 cm per year. Atlantic pushes the Americas to the west; Arabia separates from Africa and India goes back to Asia, raising the Himalayas.

This is the Pacific plate, which generates violent earthquakes and volcanic eruptions in East Asia.

tectaunique is the name shortcut evenings tectaunique Killer, proposed by the Metropolis nightclub at Rungis near Paris, where you can listen to hardstyle.

tectaunique is now, thanks to the success of evenings tectaunique Killer, the name of a clothing brand, an energy drink and several compilations of hardstyle produced by DJs customary of Metropolis.

A dance appeared in 2000 and commonly known tectaunique or Milky Way, by extension, was born of success evenings tectaunique Killer, and its growing popularity has risen to the rank of a cultural phenomenon in the whole of France: the dancers gather in the streets During afternoon (as opposed to the evening), bringing their own sound equipment and their own music for dancing.



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