What Do the Outer Planets Have in Common?

The four planets beyond the asteroid belt—Jupiter, Saturn, Uranus, and Neptune—are collectively known as the Jovian planets, named after the largest among them. These giant worlds represent a distinct class of solar system object, fundamentally different from the rocky terrestrial planets closer to the Sun. Their immense scale and unique composition result in a shared set of characteristics that govern their structure, atmosphere, and surrounding systems.

Gaseous Composition and Internal Structure

The most defining feature of the Jovian planets is their lack of a solid surface, as their outer layers are composed of deep, dense atmospheres that gradually transition into fluid interiors. Jupiter and Saturn are classified as Gas Giants because they are overwhelmingly dominated by the lightest elements, mainly hydrogen and helium, a composition reminiscent of the early solar nebula. Below the upper atmosphere, the immense pressure on Jupiter and Saturn compresses hydrogen into a state known as liquid metallic hydrogen, which acts as an electrical conductor.

Uranus and Neptune, however, are known as Ice Giants, reflecting a greater proportion of heavier elements compared to their larger neighbors. Their interiors contain significant amounts of “ices,” which are volatile compounds such as water, methane, and ammonia. The pressure within all four planets is so extreme that these materials do not exist as simple liquids or gases but rather as super-pressurized fluids.

Despite their vast, fluid envelopes, all four Jovian planets are believed to possess small, dense central cores. These cores are composed of rock and metal, similar in material to the terrestrial planets, but are much smaller in proportion to the overall planetary radius.

Massive Scale and Low Density

Jupiter, the largest, has a diameter roughly 11 times that of Earth, and even the smallest, Neptune, is nearly four times wider. This enormous size is directly related to their formation, as their powerful gravitational fields allowed them to capture vast quantities of the lightweight gases present in the outer solar system.

This composition of light elements results in a surprisingly low average density across the group, especially when compared to the dense, rocky inner planets. Saturn holds the record for the lowest density of any planet in the solar system, with a mean density less than that of water. If a bathtub large enough could hold it, Saturn would actually float.

Jupiter is the densest of the four, having a density about twice that of Saturn, a difference explained by its greater mass. Jupiter’s gravity compresses its entire volume more effectively, squeezing the hydrogen and helium into a tighter configuration. The Ice Giants, Uranus and Neptune, are slightly denser than Jupiter and Saturn because of their higher proportion of heavier, compressed icy materials.

Shared Atmospheric and Satellite Systems

Their rapid rotation rates, which complete a day in just 10 to 17 hours, drive powerful jet streams and create distinct banded cloud patterns. These atmospheric flows give rise to enormous, long-lived storm systems, such as Jupiter’s Great Red Spot, which is larger than Earth.

The visible atmospheres of Jupiter and Saturn are characterized by clouds of ammonia and water ice, while the deep blue and blue-green hues of Neptune and Uranus are caused by methane gas absorbing red light. All four planets also possess complex ring systems, a feature common to the Jovian family. Although Saturn’s rings are the most spectacular and well-known, Jupiter, Uranus, and Neptune each have fainter, darker rings composed of countless small particles of ice and rock.

Beyond their rings, all four planets host extensive families of natural satellites, or moons, with dozens orbiting each giant world. These satellite systems often resemble miniature solar systems, and many of the larger moons are composed of rock and water ice. Notable examples include Europa, a moon of Jupiter that may harbor a subsurface ocean, and Saturn’s Titan, the only moon with a dense atmosphere.

All Jovian planets generate powerful magnetic fields, which are produced by the movement of electrically conductive fluids deep within their interiors. These strong magnetic fields create vast magnetospheres that trap charged particles from the solar wind, extending far out into space. The magnetic fields of Jupiter and Saturn are particularly intense due to the churning layer of liquid metallic hydrogen that fills a significant portion of their internal structure.