From Icy Oceans to Volcanic Surfaces: The Diverse Moons of Our Solar System

Every Moon in the Solar System Explained in 5 Minutes · 5:06 · Video: Mr. Ask · Watch at the source

In short: Moons are far more than just rocky satellites. They range from lumpy, dark bodies destined to collide with their planets to massive worlds with hidden oceans. Explore how these natural satellites formed, why they are named after myths and poetry, and what makes each one unique.

Most moons in our solar system are solid bodies with very thin or non-existent atmospheres. They likely originated from discs of gas and dust that circulated around planets during the early formation of the solar system. However, some moons were likely captured by the massive gravitational fields of larger planets as they grew. This diverse range of origins explains why we see such varied geological features, including volcanic surfaces and icy oceans, across different planetary systems.

The naming conventions for these satellites reflect human culture. Most significant moons are named after mythological characters from various cultures, such as the Norse giant Bergelmir orbiting Saturn. Uranus is a notable exception; its moons are named after characters from William Shakespeare's plays, like Ophelia and Puck, or figures from Alexander Pope's poetry, such as Belinda and Ariel. When new moons are discovered in the modern era, they are assigned a numerical designation first before receiving an official name.

The inner and outer solar systems show a stark contrast in lunar populations. The terrestrial planets Mercury and Venus have no moons, while Earth has one and Mars has two small, lumpy satellites: Phobos and Deimos. In contrast, the gas giants Jupiter and Saturn, along with the ice giants Uranus and Neptune, host dozens of moons each. Mars' moon Phobos is currently spiraling inward and may collide with the planet or be torn apart into a ring within 40 to 50 million years.

Earth's Moon provides a specific case study in formation. Earth's Moon probably emerged around 4.5 billion years ago—matching the oldest lunar samples' age—following a collision between our planet and a Mars-sized object. This massive impact ejected material into orbit, which eventually accumulated to form the Moon we see today. This history was further explored by twelve American astronauts during NASA's Apollo program between 1969 and 1972.

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