Deimos (moon)

Deimos is a moon of Mars.

It is a small, gray rock. It is smaller than the other moon, Phobos.

It stays far away from the red planet. Deimos has many holes on its surface. These holes are called craters.

You could jump very high on this moon. A single jump could even send you into space! It is a very strange and cool place.

Deimos is a moon of Mars.

It is the smaller and outer of the two moons. The other moon is named Phobos. Asaph Hall found Deimos in 1877.

He was looking for moons around Mars at that time.

Deimos is a gray, rocky body. It is not a perfect circle. It has a bumpy shape. The surface has many holes called craters. Two craters have special names. They are Swift and Voltaire. They are named after famous writers.

Scientists wonder how Deimos began. Some think it was an asteroid caught by Mars. Others think it came from a larger object that broke apart.

New data from the InSight mission suggests a shared parent body. This body may have shattered long ago.

Deimos has very little gravity. This means it does not pull on things very hard. If you jumped on Deimos, you might fly into space! A single jump could reach the escape velocity. That is the speed needed to leave the moon's pull.

From Mars, Deimos looks like a tiny star.

Deimos is a small, gray moon orbiting the planet Mars. It is the outer of the two natural satellites that circle the red planet.

Its name comes from the Ancient Greek god of dread and terror. This name was suggested by a scholar named Henry Madan. He found the idea in a famous old book called the Iliad. In that story, the god Ares calls upon Dread and Fear.

Because it is so far from Mars, it is harder to see than its sibling, Phobos.

Scientists are still trying to figure out how Deimos was made. One idea is that it was an asteroid captured by Mars. This would mean a rock from the asteroid belt drifted too close and got stuck in orbit. Another idea is that the moons formed right where they are now. Some think a giant collision once filled Mars with many small moon-sized objects. Recently, researchers suggested that Deimos and Phobos might have come from one large parent body. They think this body was hit by something and shattered 1 to 2.7 billion years ago.

Asaph Hall discovered Deimos on August 12, 1877. He was working at the United States Naval Observatory in Washington, D.C. Hall was specifically searching for moons around Mars at that time. He found Deimos at about 07:48 UTC. Not long after, he also discovered the other moon, Phobos.

His discovery changed how we understand the Martian system forever.

Deimos has a very interesting shape and surface. It is not a perfect sphere but is shaped more like a lumpy rock. It is about 57% the size of Phobos. The moon is covered in craters, but its surface is smoother than Phobos because of regolith. Regolith is a layer of loose, dusty material that fills in the holes.

Two specific craters are named Swift and Voltaire after famous writers. Deimos also has very weak gravity. The escape velocity is only 5.6 meters per second. This means a person could theoretically fly into space just by jumping vertically!

If you stood on Mars, Deimos would look very different than our Moon. It would appear as a tiny, bright dot, almost like a star.

It moves through the sky slower than Mars rotates. This means it rises in the east and sets in the west. Sometimes, Deimos passes directly in front of the Sun.

This event is called a transit, and it looks like a small black dot crossing the Sun's face. Spacecraft like Opportunity and Spirit have even taken photos of this happening.

Deimos is the smaller and outer of the two natural satellites orbiting the planet Mars. Its sibling is the moon Phobos, which orbits much closer to the red planet.

Deimos is a gray-colored body with a mean radius of approximately 6.2 kilometers. It takes about 30.3 hours to complete one full orbit around Mars. Because it is located so far from its parent planet, it is much harder to observe than Phobos. The moon's name comes from the Ancient Greek god who personified dread and terror. This name was suggested by the academic Henry Madan. He drew the name from Book XV of the Iliad, where the god Ares summons Dread and Fear.

Scientists have several competing hypotheses regarding the origin of the Martian moons. One major theory is that Deimos was a captured object from the asteroid belt. This would mean an asteroid drifted near Mars and became trapped by its gravity. To stay in a circular orbit, the object would have needed to lose energy through atmospheric drag or tidal forces. Another hypothesis suggests that the moons formed exactly where they are today through accretion. A third idea proposes that a massive collision with a planetesimal once surrounded Mars with many small bodies.

In 2021, researchers proposed a new model based on seismic and orbital data. They suggest that Deimos and Phobos were born from the disruption of a single, larger parent body. This common progenitor may have been shattered by an impact between 1 and 2.7 billion years ago.

Asaph Hall III was the astronomer responsible for the discovery of Deimos. He was working at the United States Naval Observatory in Washington, D.C. Hall was specifically searching for Martian moons at the time. He discovered Deimos on August 12, 1877, at approximately 07:48 UTC. Shortly after this discovery, he also found Phobos.

His work provided the first clear evidence that Mars possessed a satellite system. While most moons in our solar system have official symbols, Deimos does not have a widely used one in astronomical literature. However, software engineer Denis Moskowitz once proposed a symbol combining a Greek delta with a spear.

Physically, Deimos is a highly non-spherical body with triaxial dimensions. It is composed of rock that is rich in carbonaceous material. This composition is very similar to C-type asteroids and carbonaceous chondrite meteorites. The surface is covered in craters, but it appears smoother than Phobos due to regolith. Regolith is a layer of loose, porous dust that partially fills the impact craters.

Two specific geological features have been named: the craters Swift and Voltaire. These are named after writers who predicted the existence of Martian moons before they were actually found. Deimos has a very low escape velocity of only 5.6 meters per second. This means a human could theoretically reach space by performing a vertical jump.

Observation of Deimos from the surface of Mars would be quite unique. To a naked-eye observer on Mars, Deimos would look like a small, bright star. Its angular diameter is no more than 2.5 minutes, which is only one-twelfth the width of our Moon seen from Earth.

Unlike Phobos, which rises in the west and sets in the east, Deimos rises in the east and sets in the west. This happens because Deimos orbits slower than Mars rotates. The moon's orbit is also slowly increasing in size due to tidal acceleration. Eventually, it is expected to escape the gravity of Mars entirely.

Deimos also performs regular solar transits as viewed from the Martian surface. A transit occurs when the moon passes directly in front of the Sun. Because Deimos is small, it does not cause a total eclipse. Instead, it appears as a small black dot moving across the solar disk.

The Mars rovers Opportunity and Spirit both photographed these events in March 2004. These observations help scientists study the moon's movement and the Martian environment. Recent data from the Mars Hope orbiter has challenged the asteroid capture theory. These new observations suggest a basaltic planetary origin for the moon instead.

Humanity has proposed many missions to explore Deimos and bring its secrets to Earth. The Aladdin mission was a finalist in the NASA Discovery Program to collect samples from the moons. Other concepts include the Hall mission and the Gulliver mission, which aims to return 1 kilogram of material. The JAXA MMX Mission is currently planned for launch in October 2026. This mission will perform flybys of Deimos to investigate its structure. Exploring Deimos could also serve as a vital step for humans traveling to Mars. The moon's dust might even be used for aerobraking during future space colonization efforts.