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Plate Tectonics - Basic explanation

 

The Earth's crust cracked into huge sections called Plates. These vast rigid plates, 100 to 150km in some places, move, albeit very slowly, due to convection currents in the mantle below the crust. The three movements these plates adopt as shown in the picture below, are - plates sliding past each other (Transform Boundaries), plates moving apart from each other (Divergent Boundaries), and plates pushing towards each other (Convergent Boundaries). Each of these movements can cause major events around the world. With little or no warning, an earthquake or volcanic eruption can unleash bursts of energy far more powerful than anything we can generate.



Transform boundaries -- where crust is neither produced nor destroyed as the plates slide past each other.

When plates slide past each other, stresses and strains build up in the Earth's crust. This may cause the plates to bend. In some cases, the stresses and strains are released suddenly, the Earth moves and the ground shakes violently in an earthquake. During an earthquake the ground breaks as the earth moves. These breaks are called Faults.

 

Divergent boundaries -- where new crust is generated as the plates pull away from each other.

When plates move apart, cracks appear in the Earth's crust. The hot molten rock escapes through the cracks, and erupts as a volcano in a shower of dust, smoke,and burning liquid. As the plates move further apart, surface rocks sink forming vertical faults. When two vertical faults occur alongside each other, Rift Valleys are formed. Most of the volcanos in the world have never been seen. They lie deep under the oceans where plates are moving apart.

 

Convergent boundaries -- where crust is destroyed as one plate dives under another.

When plates push towards each other and collide, rocks are squeezed together. Along the western edge of South America, the Nacza plate is being pushed against the South American plate. This is pushing up the land mass and creating the Andes Mountains. The last phase in the tectonic cycle occurs when two land masses collide and the ocean between them disappears. When this happens, layers of the Earth's crust are squeezed into folds. Over millions of years, mountains and valleys are formed. This happened when the Indo-Australian plate moved north and collided with the Eurasian plate. The ancient Tethys Ocean disappeared and the Himalayas was formed.

 

A bit of history

In 1912 a German scientist Alfred Lother Wegener studying an atlas, realized that the west coast of Africa was a good fit with the east coast of South America. He was aware that sufficient evidence existed to suggest that a huge ice sheet at one time covered most of South Africa, Southern Australia, and India. It was his supposition that all the Continents at one time formed a single Continent, which he called Pangaea (Greek for "all the Earth"). The theory is that around 225 million years ago pangaea lay near the South Pole. Since then, due to what he called "Continental Drift", the Continents have been drifting apart. He accounted for this movement by the explanation (since proven to be correct) that the Continents were giant blocks or plates floating and moving on the liquid mantle below the Earth's crust. The theory of continental drift would become the spark that ignited a new way of viewing the Earth. But at the time Wegener introduced his theory, the scientific community firmly believed the continents and oceans to be permanent features on the Earth's surface. Not surprisingly, his proposal was not well received.

 

Wegener's "Continental Drift"

 

225 million years ago
200 million years ago
135 million years ago
65 million years ago
Present Day

 

Alfred Lother Wegener froze to death in 1930 during an expedition crossing the Greenland ice cap. However, after his death, new evidence from ocean floor exploration and other studies rekindled interest in Wegener's theory, ultimately leading to the development of the theory of plate tectonics.

 

"Are Tectonic plates dishwasher safe?"

 

 

Colour plates by courtesy of USGS Information Services

 

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