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Last update: August 13, 2025

Quaoar: The Dwarf Planet Defying the Roche Limit with its Rings

Quaoar

Discovery and Orbital Characteristics

Quaoar, officially designated (50000) Quaoar, is a dwarf planet located in the Kuiper Belt. Discovered in 2002 by astronomers Chad Trujillo and Michael Brown, it orbits the Sun at an average distance of \(43.7\) astronomical units (AU). With a diameter of about \(1110\) km, Quaoar is one of the largest known trans-Neptunian objects.

Table of major dwarf planet objects
ObjectDiameter (km)Semi-major axis (AU)Particularities
Pluto2376 ± 339.485 satellites including Charon, nitrogen/methane atmosphere
Eris2326 ± 1267.78Albedo 0.96 (brightest), satellite Dysnomia
Haumea1560 × 1012 × 85243.13Rotation in 3.9 h (ellipsoidal shape), 2 satellites
Makemake1430 ± 945.79Methane/ethane surface, no detected atmosphere
Gonggong1230 ± 5067.38Slow rotation (22.4 h), satellite Xiangliu
Quaoar1110 ± 543.69Ring system, satellite Weywot
Sedna995 ± 80506Perihelion at 76 AU, orbital period ≈ 11,400 years
Ceres940 × 932 × 8522.77Water in the form of ice, bright spots (salts)
Orcus910 ± 2539.40Satellite Vanth, composition similar to Pluto

The Mystery of Quaoar's Rings

In 2023, an international team announced the surprising discovery of a ring system around Quaoar. These rings are located at a distance of \(4057\) km from the center of the dwarf planet, well beyond the Roche limit, where tidal forces should prevent the formation of such structures. This discovery challenges our current models of ring formation and stability.

Possible Origin of the Rings

Several hypotheses are put forward to explain the formation of Quaoar's rings:

Summary: The Puzzle of Quaoar's Rings

The recently discovered rings around the dwarf planet Quaoar pose a physical challenge related to their formation, composition, and stability. Their existence relies on a complex dynamic balance between Quaoar's gravity, tidal forces (notably the Roche limit), and interactions between particles.

Several hypotheses explain their origin: debris from collisions, disintegration of a nearby satellite, or accumulation of dust. The stability of the system depends on internal collisions, gravitational resonances with potential small shepherd satellites, and non-gravitational effects such as solar radiation pressure.

The particles making up these rings are mainly composed of water ice and organic materials, with sizes ranging from microns to centimeters.

Articles on the same theme

Dwarf Planets: The Forgotten Worlds of the Solar System Dwarf Planets: The Forgotten Worlds of the Solar System
Physical Composition of Trans-Neptunian Objects in the Kuiper Belt Physical Composition of Trans-Neptunian Objects in the Kuiper Belt
Haumea and its Moons: A Singularity of the Solar System Haumea and its Moons: A Singularity of the Solar System
The Enigma of the Oort Cloud: Indirect Evidence and Uncertainties The Enigma of the Oort Cloud: Indirect Evidence and Uncertainties
Solar System Ice Line Solar System Ice Line
Sedna, the goddess of the frozen oceans Sedna, the goddess of the frozen oceans
Roche limit Roche limit
Hadean's Hell Hadean's Hell
Quaoar: The Dwarf Planet Defying the Roche Limit with its Rings Quaoar: The Dwarf Planet Defying the Roche Limit with its Rings
The 40 largest objects in the solar system The 40 largest objects in the solar system
Pluto's Satellites: Strange Companions in the Dwarf Planet's Shadow Pluto's Satellites: Strange Companions in the Dwarf Planet's Shadow
Ceres: Boundary Between Asteroid and Dwarf Planet Ceres: Boundary Between Asteroid and Dwarf Planet
Pluto and its Moons: Charon, Nix, Hydra, Styx, and Kerberos Pluto and its Moons: Charon, Nix, Hydra, Styx, and Kerberos
Simulator, the round of near-Earth cruisers Simulator, the round of near-Earth cruisers
Eris, the dwarf planet and its highly inclined orbit Eris, the dwarf planet and its highly inclined orbit

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