The Moon Is Older Than Scientists Thought





Mindblower, 16 Jan - 2017 ,

The Moon Is Older Than Scientists Thought
Credit: almanac.com

A UCLA-led research team reports that the moon is at least 4.51 billion years old, or 40 million to 140 million years older than scientists previously thought.

A UCLA-led research team reports that the moon is at least 4.51 billion years old, or 40 million to 140 million years older than scientists previously thought.

The findings - based on an analysis of minerals from the moon called zircons that were brought back to Earth by the Apollo 14 mission in 1971 - are published Jan. 11 in the journal Science Advances.

The moon's age has been a hotly debated topic, even though scientists have tried to settle the question over many years and using a wide range of scientific techniques.

"We have finally pinned down a minimum age for the moon; it's time we knew its age and now we do," said Mélanie Barboni, the study's lead author and a research geochemist in UCLA's Department of Earth, Planetary and Space Sciences.

The moon was formed by a violent, head-on collision between the early Earth and a "planetary embryo" called Theia, a UCLA-led team of geochemists and colleagues reported in 2016.

The newest research would mean that the moon formed "only" about 60 million years after the birth of the solar system - an important point because it would provide critical information for astronomers and planetary scientists who seek to understand the early evolution of the Earth and our solar system.

That has been a difficult task, Barboni said, because "whatever was there before the giant impact has been erased." While scientists cannot know what occurred before the collision with Theia, these findings are important because they will help scientists continue to piece together major events that followed it.

It's usually difficult to determine the age of moon rocks because most of them contain a patchwork of fragments of multiple other rocks. But Barboni was able to analyze eight zircons in pristine condition. Specifically, she examined how the uranium they contained had decayed to lead (in a lab at Princeton University) and how the lutetium they contained had decayed to an element called hafnium (using a mass spectrometer at UCLA). The researchers analyzed those elements together to determine the moon's age.


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