Home Random Thoughts Short pieces Long pieces Talk to Me

Long pieces

THE UNIQUE EARTH AND GEOMORPHOLOGY ( Page 2 )

Land Ahoy
Meanwhile there was constant flow of heat from the very hot interior to the exterior. This was not conducted away to the outside, as the lithosphere was a poor conductor. Hence the excess energy found outlet through vents of volcanism. This gradually built mid oceanic ridges and in the southern hemisphere some of the lithosphere rose above the water, creating the first islands or an archipelago. Still there was no continent or a landmass of any considerable size. For more than three billion years our planet remained a huge ocean, with some islands and frozen water around the pole. The first super continent was formed some 700 million years ago, most of the land being in the southern hemisphere. Geologists call this landmass Pangaea.
A Jigsaw Puzzle
We have got used to the idea that the earth is rotating on its axis rather fast and flying round the sun every year. And now comes this notion that the surface of the earth is not at rest at all. The continents are always moving ever so slightly, some very slow, others comparatively fast. The branch of geomorphology called plate tectonics dealing with the movements of continental plates and ocean plates was born in the fifties. About 200 million years ago the single continent of Pangaea started breaking up. 180 million years ago there were two landmasses the northern one called Laurasia and the southern one Gondwanaland. These two were still nominally joined at Gibraltar. Then Gondwanaland began breaking up. About 130 million years ago, Africa, retaining South America, Arabia and Madagascar began moving north, away from the southern most landmass comprising of Antarctica and Australia as a single piece. Later the Indian plate also had broken up from Africa and began moving north. The present island of Madagascar was joined with the Indian plate.
65 million years ago South America broke off from Africa. The Madagascar separated from the Indian plate. The Indian plate reached the equator in its flight to join Asia. Africa disengaged from Europe at Gibraltar but a new link to Asia was made at Suez, though Arabia was still part of the African landmass. Australia was still joined to Antarctica though the Australian section had moved further north. While all these changes were happening in the southern hemisphere, the northern part, Laurasia seemed to have undergone very little change. Though this part began breaking up, the Canadian section was still fully joined to the western European section. The various pieces of the Jig saw puzzle on the earth’s crust was placed in their present positions during the last 50 million years. There were some very remarkable events in this relatively short span of time in earth’s history.
During this period:
1) North America broke off from Europe and joined up with South America.
2) Australia broke off from Antarctica and moved further north
3) The fault line that created east African rift valley system also created the red sea separating Arabia from Africa except for the Suez connection.
4) This period also saw the birth of many of the present islands including all the islands of the South-East Asia, the British Isles and Sri Lanka. One of the youngest islands is the Hawaii.
5) The Indian plate moving up north joined up with the Asian landmass
Of all these the most dramatic event was the fusion of the Indian plate with the Asian continental mass. The force of this collision gave birth to the rise of the greatest mountain range in the world, the Himalayas. It was also this event that gave rise to a new climatic phenomenon, the monsoons. According to some geologists, the Indian plate is still moving northwards at a rate of something like 2 cm per year. Is this going to push the Himalayas and Everest still higher than it is now. Not likely. They suggest that the Indian plate is sliding under the continental mass and the result could be catastrophic earthquakes that could affect many densely populated areas from Kashmir to the Ganges delta.