The ‘Roof of the World’ appears to have risen by up to 600 meters [1,968.5 feet], new research indicates.
Tibet is referred to as the Roof of the World for good reason. With an average altitude of 4,500 meters [14,763.78 feet] above sea level and the world’s two highest peaks, Mount Everest and K2, the vast Himalayan mountain range towers higher than anywhere else on Earth.
But the Tibetan plateau’s height has been the subject of academic controversy for many years. Some researchers believe that the area has been as high as it is today for most of its existence, while others believe that the area has increased in height over the past 20–30 million years. It is a riddle that until recently has remained unsolved.
With the help of new analyses of the Indian Ocean seabed and calculations of the movement of Earth’s tectonic plates, the new research contributes new answers to the disagreement.
“By looking at older data of Tibet’s emergence and combining it with new geological data from the Indian Ocean, we are pretty certain that there was a major geological change in Tibet about 15-18 million years ago, one that caused the wide area to rise between 300 and 600 meters,” explains the study’s main author Giampiero Iaffaldano, an associate professor in the geosciences and natural resource management department at the University of Copenhagen.
The change is due to a head on collision between what are today India and China. India was originally located much further south, but the tectonic plate upon which India lies gradually moved northwards over millions of years and closer to China, until they finally collided to form Tibet.
Using plant fossils and geochemical analyses of rocks found in the mountainous region, some scientific researchers have been quite sure that Tibet looked the way it does today as far back as 20–30 million years ago and that its altitude has not changed over time.
Other researchers have believed that the prolonged and decelerating collision between India and China was caused by Tibet shooting upwards as much as two kilometers (about 1.24 miles) over a few million years. But according to Iaffaldano, the answer is found somewhere in between.
“What the study contributes to is actually a combination of the two previous hypotheses, different data sets and conclusions. What I’ve done is take a closer look at the speed of the India-China collision using Indian Ocean geological data that has only recently become available to the public,” he says.
Continuously through time, hot stones and other material are spat from Earth’s interior onto the ocean floor. They have much to reveal about the movements of Earth’s tectonic plates. Encoded within these lavas are records of Earth’s magnetic polarity—the direction of Earth’s north and south poles.
Polarity has reversed several times in Earth’s history, meaning that North has become South and vice-versa. And, scientific researchers know roughly when these flips occurred. As such, they can trace tectonic plates to specific places and times during Earth’s history using their magnetization along a so-called geomagnetic timescale.
“A closer look at this type of data held the answer to the question of whether Tibet has gotten higher or not. It has proven tremendously useful to calculate the speed of India’s collision with China from geomagnetic data. More and more of such data, often originally collected for purposes other than fundamental scientific research and thereby not publicly available, is now being released and used by scientists,” explains Iaffaldano.
“This new knowledge about Tibet is important for better understanding of Earth’s evolution and the methods used could turn out useful in future studies.”
The research appears in Geophysical Journal International.
Source: University of Copenhagen