TNPSC Thervupettagam

The Gamburtsev Mountains

May 17 , 2025 13 hrs 0 min 54 0
  • The Gamburtsev Mountains are similar in scale and shape to the European Alps.
  • They are buried beneath the highest point of the East Antarctica ice sheet.
  • Plate tectonic models suggest the crust now forming East Antarctica came from at least two large continents more than 700 million years ago.
  • As per the zircon grains analysis, the Gamburtsev Mountains began to rise around 650 million years ago, reached Himalayan heights by 580 million years ago.
  • Then it experienced deep crustal melting and flow that ended around 500 million years ago.
  • Zircons are often called “time capsules” because they contain minuscule amounts of uranium in their crystal structure.
  • The uranium decays at a known rate and allows scientists to determine their age with great precision.

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