Logo Genista, fondé en 1971

Tectonics : the Earth quakes [1]

Tectonique : la Terre tremble [1] Vous pouvez aussi lire cette page en français : Cliquez ici

The Earth : Our planet is living - Its quakes [Genista]

By Nicolle Mathé, 'Genista Informations' No. 293, May 2003 (Plate tectonics)

the Earth [la Terre] The Etna is turbulent, as are its nearby neighbours, the Stromboli and the Vulcano -- and the Vesuvius gives unrest. The Earth quakes here and there in the Alps, the Pyrenees, Turkey, Greece...
Lots of questions justle about : is there a link between all these events ? Can one foresee the places and yimes of these tremblings ? Will our Mediterranean sea, that we ill-treat so much, exist forever ?
section of the Earth from the surface down to the centre [coupe de la Terre de la surface jusqu'au centre]

A slice of globe


Our earthly sphere spreads its two major components in front of our eyes :

 Rocks more or less hard, arranged in layers which we can see, so irregular in shape, in our mountains.
Their erosion gives the thin elements in our soil, which are the basis of our cultures and constructions.
They form a superficial layer, the Earth's crust, called lithosphere — from the Greek lithos = 'stone'

 Some molten viscous rocks, or lava, at a temperature of 900-1200°C, which gush out and pour out through cracks made in the underlying layers, until they build up impressivee structures such as aerial or underwater volcanoes.
It comes from a low-viscosity magma, located under the lithosphere and constituting the asthenosphere — from the Greek asthenes = 'weak'.




A heterogeneous crust


The crust, in fact, has naither the same composition, nor the same thickness, depending on the various places :

The oceanic floors are essentially constituted of basalt and are not very think — 6 to 19 miles (10 to 30 km).

The continental blocks are made of varied sedimentary, metamorphic and granitic rocks. Their thickness ranges from 31 miles (50 km) in plains to 62 miles (100 km) in mountain areas.




the tectonic plates of our planet Earth [les plaques tectoniques de notre planète Terre]

A discontinuous crust


The crust is not an envelope of one piece.
It is cracked through all its thickness and along impressive distances.
Those cracks encompass pieces called tectonic plates — from the Greek tektonikos = 'which concerns construction'.

Tectonics - In this series


* TECTONICS : THE EARTH
(1) Our planet is living : its quakes (The present Page)
(2) Drift away, plates : the drift
(3) It folds or it breaks : an active planet

* TECTONICS : THE MEDITERRANEAN SEA
(4) The Mediterranean Sea : a jigsaw puzzle
(5) In the Mediterranean Sea : meditate...



Top of Page  •  [Haut de Page]

Cette Page en français  •  [This Page in French]

Part 2 : Drift away, plates - The drift  •  [Deuxième Partie : Voguent les plaques - La dérive]

Part 3 : It folds or it breaks - an active planet  •  [Troisième Partie : Ça plisse ou ça casse - Planète active]

Contents : Nature & Environment  •  [Sommaire Nature & Environnement]