New Discoveries From Ancient Rocks
Over the last few years, improved technology has teased new secrets out of the Apollo-era moon rocks — and shed new light on the long-vanished but now-confirmed lunar magnetosphere. Not only did the moon once have a magnetosphere, but it may have played a significant role in protecting Earth’s atmosphere.
The atmospheres of the solar system’s inner planets are subject to erosion from the powerful solar winds of fast-moving particles. These particles collide with atmospheric atoms, hitting them with such force that they can exceed the planet’s escape velocity and go hurtling through interplanetary space.
The dense atmosphere of Venus has resisted such erosion, but Mars lost most of its atmosphere — along with the seas it once had, as the water either froze in the thin cold air or evaporated.
Earth’s atmosphere and oceans have been protected by its magnetic field, which deflects the charged particles from the sun, keeping most of them from hitting and eroding the atmosphere.
A Complex History of Lunar Magnetism
Scientists now believe that, in the early days of the solar system, the lunar magnetosphere contributed to this protection. Indeed, according to NASA, from about 4.1 to 3.5 billion years ago, the Earth’s and moon’s magnetic fields were linked, providing a duo of magnetic fields protecting the Earth-moon system.
What’s most surprising is that, in that era, the lunar magnetosphere was actually more powerful than Earth’s is today, as MIT News reports. The current strength of Earth’s magnetosphere is about 50 microteslas, while the ancient lunar magnetosphere may have pegged the needle at up to 100 microteslas in strength.
By 2.5 billion years ago, this powerful field had faded to no more than 10 microteslas. And by the time the youngest moon rocks were formed — by an asteroid impact about a billion years ago — the magnetic field had faded to no more than 0.1 microteslas or possibly to nothing.
This gradual and uneven fade suggests that more than one mechanism contributed to the early lunar magnetosphere. In the early period, when the field was strongest, the moon orbited much closer to Earth and was subjected to powerful tidal forces that could have kept the lunar interior churned up enough to produce a strong magnetic field.
As the moon’s orbit crept outward, these tidal forces weakened, but lunar vulcanism persisted, showing that the moon’s interior had not yet fully crystallized and was still fluid enough to produce a weak magnetic field. Finally, the moon froze solid, and its magnetic field faded, leaving only the traces in moon rocks that puzzled Apollo-era researchers.
But the fact that Earth once had a magnetic moon has implication for the search for life on extrasolar planets. The atmospheres of these distant worlds may have been protected not only by their own magnetospheres but also by the fields of any large moons orbiting them.
And, closer to home, we can also wonder what other surprises the moon has in store, waiting for us to discover when we return.
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