• Recently, some researchers studied a meteorite from Katol, Maharashtra which was from the meteor shower of 2012.
  • A meteorite is a solid piece of debris from an object, such as a comet, asteroid, or meteoroid, that originates in outer space and survives its passage through the atmosphere to reach the surface of a planet or moon.

Important points:

  • Initial studies revealed that the host rock was mainly composed of olivine, an olive-green mineral.
  • Olivine is the most abundant phase in our Earth’s upper mantle.
  • Earth is composed of different layers including the outer crust, followed by the mantle and then the inner core
  • It was believed that we can reach the upper mantle if we drill for about 410 kilometers.
  • However, by studying the composition of these meteorite fragments, researchers have unravelled the composition expected to be present in the Earth’s lower mantle which is at about 660 km deep.
  • Various computational and experimental studies have shown that about 80% of the Earth’s lower mantle is made up of bridgmanite. By studying this meteorite sample, scientists can decode how bridgmanite crystallized during the final stages of our Earth’s formation.
  • Bridgmanite is a magnesium-silicate mineral, MgSiO3, the most abundant mineral on earth.
  • The mineral was named in 2014 after Prof. Percy W. Bridgman, recipient of the 1946 Nobel Prize in Physics.
  • As the bridgmanite of the Katol meteorite sample closely matches with the bridgmanite on Earth.
  • The bridgmanite in the meteorite was found to be formed at pressures of about 23 to 25 gigapascals generated by the shock event.
  • The high temperature and pressure in our Earth’s interior have changed over billions of years causing crystallisation, melting, remelting of the different minerals before they reached their current state.


  • Studying the meteorite could also tell us more about how our Earth evolved from being a magma ocean to a rocky planet and researchers can unearth more details about the formation of Earth.
  • It is important to study these individual minerals to get a thorough idea of how and when the Earth’s layers formed.
  • Scientists can also decode how bridgmanite crystallized during the final stages of our Earth’s formation.


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