 |
|
A picture of Mount Qomolangma.
|
Will the Himalaya Mountains, home to the world's highest peaks, continue to push up into the sky in future? Some Chinese scientists say no.
The Himalayas may have reached their highest altitude and in the centuries to come may even shrink a little, said Bian Qiantao, a researcher with the Institute of Geology and Geophysics of the Chinese Academy of Sciences.
Located on the southern rim of the Qinghai-Tibet Plateau, the Himalaya Mountains form an arc protruding southward. The main part of the range lies in China. "Himalaya" means "abode of snow" in Tibetan. The average height of these mountains is more than 6,000 metres.
Scientists believe that 65 million years ago, the Indian Plate moving north collided with theEurasian Plate, and the upheaval saw the emergence of the Qinghai-Tibet Plateau as well as the Himalayas.
"Friction between the tectonic plates continues to this day, gradually pushing the Himalayas upward," said Bian.
"But at the same time, a horizontal pulling power inside the lower continental crust and mantle of the earth counteracts this upward movement," said Bian.
According to measurements made by scientists in 2005, the altitude of Mount Qomolangma is 8844.43 metres, 3.70 metres lower than the figure obtained in 1975.
The result suggests that the Himalayas and the Qinghai-Tibet Plateau will not continue to move up indefinitely. After growing to a certain height, the effect of gravity and collision-generated extrusion will make them grow wider, but not higher, Bian said.
點擊進入往期回顧
(China Daily)
|
擁有世界最高峰的喜馬拉雅山還將繼續(xù)“長高”嗎？我國一些科學(xué)家認(rèn)為“不會”。
中科院地質(zhì)與地球物理研究院的研究員邊千韜說，喜馬拉雅山已基本達(dá)到最高點，在未來幾個世紀(jì)內(nèi)，甚至可能會有所下降。
喜馬拉雅山位于青藏高原南側(cè)，呈向南突出的弧形，山脈的主要部分位于中國境內(nèi)。“喜馬拉雅”在藏語中是“冰雪之鄉(xiāng)”的意思。喜馬拉雅山的平均高度在6000米以上。
科學(xué)界普遍認(rèn)為，青藏高原和喜馬拉雅山是6500萬年前向北漂移的印度板塊與歐亞板塊相撞而形成的。
邊教授說：“這兩個板塊之間的摩擦仍在繼續(xù)，在這種力量的作用下，喜馬拉雅山一直在慢慢升高。”
“但同時，從下地殼一直到地幔上部在產(chǎn)生一種東西拉張的力量，這種拉力對喜馬拉雅山的繼續(xù)升高起到了阻礙作用。”
2005年，科學(xué)家測出珠穆朗瑪峰的海拔為8844.43米，比1975年低3.7米。
測量結(jié)果表明，喜馬拉雅山和青藏高原不會無限升高。邊教授說，喜馬拉雅山達(dá)到一定高度后，在重力和由板塊碰撞產(chǎn)生的擠壓力的作用下，山脈會向外擴展，而不會持續(xù)增高。
(英語點津姍姍編輯)
|
