Haumea
On the 28th of December 2004, a team led by Mike Brown at Caltech spotted the object that would become Haumea. They captured images on the 6th of May 2004 and published an abstract about their find on the 20th of July 2005. Just weeks later, José Luis Ortiz Moreno's team in Spain found the same object in precovery images taken between 7 and the 10th of March 2003. The Spanish group filed their discovery claim with the Minor Planet Center on the 27th of July 2005. This timing created a dispute over who deserved credit for finding the dwarf planet. Brown initially accepted Ortiz's priority but soon suspected foul play after learning the Spanish observatory had accessed his observation logs before the announcement. Those logs contained data allowing the Ortiz team to identify the object in their earlier 2003 images. The IAU eventually named the body Haumea, a Hawaiian goddess of childbirth, despite the Spanish team proposing Ataecina instead. The name chosen reflected the location where the moons were discovered rather than the discoverer's preference.
Haumea spins once every 3.9 hours, faster than any other known equilibrium body larger than 100 kilometers across. This rapid rotation distorts the dwarf planet into a triaxial ellipsoid shape. Calculations suggest its major axis is twice as long as its minor axis. If it spun much faster, the body would split apart like a dumbbell. Most rotating bodies flatten into oblate spheroids, but Haumea stretches into three unequal dimensions. Observations from January 2017 revealed dimensions of approximately 2,322 by 1,704 by 1,026 kilometers. The light curve fluctuations confirm this elongated form. Scientists believe the extreme spin resulted from a giant collision that also created its family of objects. The rotational physics predicts such distortion occurs within just one hundred days for a body spinning at this speed. The equator plane aligns nearly edge-on to Earth, complicating direct observation of its true geometry.
A massive impact shattered a progenitor body billions of years ago to create Haumea and its kin. This event ejected fragments that now orbit as moons or drift independently through space. The resulting group includes several large trans-Neptunian objects sharing similar physical traits. Brown proposed these fragments formed directly from the impact that stripped away Haumea's ice mantle. A second theory suggests the debris first coalesced into a large moon before shattering again in a secondary collision. This scenario better matches the measured velocity dispersion among family members. The collision likely occurred at least one billion years ago in the scattered disc region. Such events are rare today with less than 0.1 percent probability over the Solar System's age. The dynamic environment of the primordial Kuiper belt would have disrupted any close-knit group during Neptune's migration. Therefore, the origin point must lie in the denser scattered disc where collisions were far more frequent.
Spectra obtained by Gemini and Keck telescopes in 2005 revealed strong crystalline water ice features on Haumea's surface. Crystalline ice forms above 110 Kelvin yet Haumea's temperature stays below 50 Kelvin. Cosmic rays bombard trans-Neptunian objects constantly, converting crystalline structures back to amorphous ice within ten million years. Yet this dwarf planet has existed in its cold location for billions of years without resurfacing mechanisms. The high albedo ranges between 0.6 and 0.8, consistent with fresh crystalline ice covering most of the terrain. Some models suggest up to 80 percent of the surface consists of pure crystalline water ice. A dark red area observed in September 2009 indicates regions rich in minerals or organic compounds. The absence of ammonia hydrate rules out cryovolcanism as a recent resurfacing source. Radiation damage should redden and darken surfaces over time, but Haumea remains bright white like snow.
A stellar occultation event on the 21st of January 2017 confirmed the presence of a ring system around Haumea. This marked the first ring discovered orbiting any trans-Neptunian object or dwarf planet. The ring spans approximately 2,287 kilometers from the center with a width of about 70 kilometers. Its opacity measures 0.5, contributing roughly five percent to the total brightness of the system. The ring plane tilts relative to Haumea's equator and aligns closely with the orbital path of Hiiaka. It sits well within the Roche limit which extends to about 4,400 kilometers if the body were spherical. Particles originate near a stable region in phase space despite being close to an unstable 1:3 resonance. The ring's existence challenges previous assumptions that rings could not persist around such small bodies for long periods.
Two moons named Hiiaka and Namaka orbit Haumea at distances ranging from 25,657 to 49,880 kilometers. Hiiaka was discovered on the 26th of January 2005 while Namaka appeared on the 30th of June 2005. Both satellites likely formed from fragments ejected during the giant collision that shaped the main body. Hiiaka orbits every 49 days in a nearly circular path and measures roughly 310 kilometers across. Namaka completes its circuit in just 18 days along a highly elliptical trajectory inclined 13 degrees from the larger moon. Their mutual inclination creates unexpected orbital dynamics since tidal effects should have damped these eccentricities over time. A recent passage through a 3:1 resonance with Hiiaka may explain their current excited states. Occultation events between 2008 and 2011 provided rare opportunities to study the system's geometry from Earth. These alignments allowed precise measurements of size and shape before the viewing angle shifted permanently.
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Common questions
When was Haumea discovered and who found it?
A team led by Mike Brown at Caltech spotted the object on the 28th of December 2004. They captured images on the 6th of May 2004 and published an abstract about their find on the 20th of July 2005.
What is the shape and rotation speed of Haumea?
Haumea spins once every 3.9 hours which distorts the dwarf planet into a triaxial ellipsoid shape. Observations from January 2017 revealed dimensions of approximately 2,322 by 1,704 by 1,026 kilometers.
How did Haumea form and what created its moons?
A massive impact shattered a progenitor body billions of years ago to create Haumea and its kin. This event ejected fragments that now orbit as moons or drift independently through space.
What does the surface of Haumea look like and when was this observed?
Spectra obtained by Gemini and Keck telescopes in 2005 revealed strong crystalline water ice features on Haumea's surface. A dark red area observed in September 2009 indicates regions rich in minerals or organic compounds.
When was the ring system around Haumea confirmed and how wide is it?
A stellar occultation event on the 21st of January 2017 confirmed the presence of a ring system around Haumea. The ring spans approximately 2,287 kilometers from the center with a width of about 70 kilometers.
Who discovered the two moons of Haumea and when were they found?
Hiiaka was discovered on the 26th of January 2005 while Namaka appeared on the 30th of June 2005. Both satellites likely formed from fragments ejected during the giant collision that shaped the main body.