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Giant-impact hypothesis

Adapted from Wikipedia · Adventurer experience

An artist's illustration showing a cosmic collision between two celestial bodies near a young star, helping us learn about how planets form.

The giant-impact hypothesis, sometimes called the Theia Impact, is an astrogeology hypothesis for how the Moon was formed. It was first suggested in 1946 by Canadian geologist Reginald Daly. This idea says that long ago, about 4.5 billion years ago, the early Earth crashed into a planet about the size of Mars. This planet is often called Theia, after a mythical Greek Titan who was the mother of Selene, the goddess of the Moon.

Artist's depiction of a collision between two planetary bodies. Such an impact between Earth and a Mars-sized object likely formed the Moon.

When these two large objects collided, pieces of both were thrown into space. Over time, these pieces came together and formed the Moon we see today. Scientists support this idea because several clues fit with what we see now. The Moon’s orbit and Earth’s rotation are angled similarly, and the rocks from the Moon and Earth have almost the same chemical makeup. Also, the Earth and Moon together spin and move in a way that needs a lot of energy — the kind that could come from a big crash.

Even though this hypothesis is widely accepted among astronomers, there are still some mysteries. For example, we do not yet have a perfect model that shows exactly how the pieces from the crash came together to make the Moon. But this idea helps us understand not just our Moon, but how other star systems might form planets and moons too.

History

In 1898, George Darwin thought that Earth and the Moon were once one body. He believed the Moon was spun from Earth by strong forces.

Later, American and Soviet experiments showed that the Moon is moving away from Earth.

But Darwin's idea couldn't fully explain the Moon's origin. In 1946, Reginald Aldworth Daly from Harvard University suggested the Moon was created by a big crash. His idea wasn't popular until 1974, when William K. Hartmann and Donald R. Davis brought it up again. They thought a large object might have hit Earth, sending material into space that formed the Moon.

Around the same time, Alastair G. W. Cameron and William R. Ward proposed that a body about the size of Mars hit Earth at an angle. They believed this could explain why the Moon has less iron than Earth. In 1984, in Kona, Hawaii, the idea that a big impact created the Moon became the most popular explanation.

Theia

Main article: Theia (hypothetical planet)

Theia formed at the L4 Lagrange point, then went into a chaotic orbit, approached the Earth, and collided with it. One "loop" of the orbit takes one year. The Earth is shown stationary (rotating frame of reference).

The name of the imagined planet comes from a story about a Greek titan named Theia, who was the mother of Selene, the goddess of the Moon. This name was suggested by a scientist in the year 2000 and is now commonly used. Scientists think Theia was one of many Mars-sized objects that existed in our Solar System about 4.5 billion years ago. It is believed to have moved in a special pattern with Earth and the Sun. The giant-impact hypothesis suggests that Earth had many big collisions while it was forming, and the one that created the Moon was just one of these huge impacts.

Basic model

Simplistic representation of the giant-impact hypothesis

Astronomers believe that a big crash happened between Earth and a planet called Theia about 4.4 to 4.45 billion years ago, not long after our Solar System started. This crash happened at an angle while Earth was almost fully formed.

After the crash, pieces of both Earth and Theia were thrown into space. Some of these pieces stayed close to Earth and eventually came together to form the Moon. The crash also changed how fast Earth spins and added more material to our planet.

Composition

In 2001, scientists found that rocks from the Moon were very similar to rocks from Earth. This was different from most other objects in space.

In 2014, scientists found a small difference between Moon rocks and Earth rocks. One idea is that the object that hit Earth, named Theia, may have formed close to our planet.

These discoveries fit with the giant-impact hypothesis. This idea says that Earth crashed into a Mars-sized object about 4.5 billion years ago. The pieces from this crash later came together to form the Moon.

Evidence

Scientists have found clues that support the idea that a big crash helped create the Moon. Rocks brought back from the Moon by astronauts show that their makeup is very similar to Earth’s rocks. This suggests that the Moon formed from material that once was part of Earth. The Moon also seems to have a smaller core than most planets, which fits with the idea that a large object crashed into Earth long ago.

Studies of special elements in Moon rocks compared to rocks from Earth and Mars also back up this theory. These elements act differently when heated, and the Moon’s rocks show signs of having been heated by a big impact.

Difficulties

The idea that a big crash formed the Moon has some puzzles that scientists are still trying to solve. One puzzle is that this idea suggests Earth would have had a thick layer of melted rock after the crash, but we don’t see any signs that Earth ever had such a layer.

Composition

There are some things about what the Moon is made of that this idea doesn’t fully explain:

  • The amounts of certain elements on the Moon don’t match what we’d expect if the Moon came from a big crash.
  • Finding water and other materials on the Moon is harder to explain if the Moon formed from a very hot crash.
  • The Moon has a certain amount of iron that doesn’t quite match what we’d expect if it came mostly from Earth or another planet.
  • The Moon seems to lack some elements that we’d expect if it formed from another planet.
  • The Moon’s oxygen looks almost exactly like Earth’s, which is surprising if it came from another planet.
  • The Moon’s titanium also looks very similar to Earth’s, suggesting that not much of it came from another planet.

Lack of a Venusian moon

If the Moon formed from a big crash, we might expect other planets like Venus to have moons too. But Venus doesn’t have a big moon. One idea is that if Venus did have a moon, it might have been pulled in by the Sun or crashed back into Venus because of its closeness to the Sun. Big crashes like the one that might have formed our Moon were probably common, and they often result in a single moon. However, whether such a moon stays in orbit depends on many factors, like how far the planet is from the Sun and how the moon’s orbit is tilted.

Possible origin of Theia

In 2004, a mathematician from Princeton University and an astrophysicist thought that Theia may have formed at special spots in Earth’s path called L4 or L5 Lagrangian point, like some asteroids. As Theia grew, its path changed and it crashed into Earth.

Later studies suggested this crash may have happened a little later than we first thought. Some scientists think other objects might have been made in this crash and stayed in space for a very long time before moving away. In 2019, scientists found hints that Theia might have come from far away in our Solar System.

Alternative hypotheses

Main article: Origin of the Moon

Scientists have thought of several ways the Moon might have formed. One idea is that the Moon broke off from Earth when it was spinning very fast. Another idea is that the Moon was born somewhere else and Earth’s gravity pulled it in. Some believe Earth and the Moon formed together from the same cloud of dust and gas.

Another idea says a big space rock hit Earth later than usual, making the Moon mostly from Earth’s pieces.

A final idea, from 2012, says the Moon and Earth formed together after two big objects crashed into each other. After this crash, Earth was covered in material that eventually came together to make the Moon.

Images

A beautiful full moon shining brightly in the night sky, captured from Madison, Alabama.
NASA's GRAIL mission data reveals the topography and gravity patterns of the Moon's 'Ocean of Storms' region, showing ancient rift valleys and lava plains.
A detailed map showing gravity anomalies and ancient rift zones on the Moon's surface, created from data collected by NASA's GRAIL mission.
An artist's view of the Ocean of Storms on Earth's Moon, showing ancient lava-flooded rifts as revealed by NASA's GRAIL mission.
A stunning view of Earth rising over the lunar horizon, as seen by astronauts aboard Apollo 8.
A colorful educational montage showing the planets of our solar system—Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune—as captured by NASA spacecraft. Perfect for learning about space!
An animation showing areas deep inside the Earth where material moves slowly, helping scientists understand our planet's structure.
An artist's rendering of HE 1523-0901, one of the oldest known stars in our galaxy, located about 7500 light years from Earth.

Related articles

This article is a child-friendly adaptation of the Wikipedia article on Giant-impact hypothesis, available under CC BY-SA 4.0.

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