Skip to content
— CH. 1 · INTRODUCTION —

Ceres (dwarf planet)

~10 min read · Ch. 1 of 8
8 sections
  • Ceres sits in the main asteroid belt between Mars and Jupiter, and it has been classified as a planet, demoted to an asteroid, and upgraded again to dwarf planet, all within the span of two centuries. On the 1st of January 1801, Giuseppe Piazzi, a Catholic priest and astronomer at the Palermo Astronomical Observatory in Sicily, spotted a faint moving point of light he initially mistook for a comet. What he had actually found was an object larger than anything else in the asteroid belt, a body so rich in water ice that it may contain the most water of any object in the inner Solar System after Earth itself. How did a rocky, icy world smaller than the Moon end up at the center of so many scientific debates? What does the interior of Ceres look like, and could it support life? And why did a NASA spacecraft called Dawn travel hundreds of millions of kilometers to find out?

  • Johannes Kepler, writing in 1596, argued that the ratios between planetary orbits would only conform to what he called "God's design" if two additional planets existed: one between Jupiter and Mars, and one between Venus and Mercury. That idea simmered for nearly two centuries. In 1761, astronomer and mathematician Johann Heinrich Lambert posed the question in vivid terms, asking whether planets were missing from the "vast space between Mars and Jupiter" and whether Jupiter and Saturn were "destined to plunder forever" the weaker bodies around them.

    In 1772, German astronomer Johann Elert Bode published a mathematical formula, crediting Johann Daniel Titius, that became known as the Titius-Bode law. The formula appeared to predict the orbital distances of all known planets but left an unexplained gap between Mars and Jupiter, pointing to a missing world at roughly 2.8 astronomical units from the Sun, or about 420 million kilometers out. When William Herschel discovered Uranus in 1781 near the distance the law predicted for a planet beyond Saturn, confidence in the formula rose sharply.

    By 1800, the editor of the German astronomical journal Monatliche Correspondenz, Franz Xaver von Zach, assembled a team of twenty-four astronomers he called the "celestial police" and tasked them with a methodical search. The group never found Ceres, but they did later identify the asteroids Pallas, Juno, and Vesta. The prize had already slipped past them before their search even began.

  • Piazzi had been invited to join von Zach's celestial police, but he had not yet received his invitation when he made his discovery. He was not even hunting for the missing planet that night; he was searching for "the 87th star of the Catalogue of the Zodiacal stars of Mr la Caille" when he noticed it was "preceded by another" object that did not belong. The object moved. Over the following weeks, Piazzi observed it twenty-four times, with his final sighting recorded on the 11th of February 1801, when illness cut his work short.

    On the 24th of January 1801, Piazzi sent letters to two colleagues, his compatriot Barnaba Oriani of Milan and Bode in Berlin. He reported the object as a comet but added a telling caveat: "since its movement is so slow and rather uniform, it has occurred to me several times that it might be something better than a comet." In April he forwarded his complete observations to Oriani, Bode, and French astronomer Jerome Lalande, and the data appeared in the September 1801 issue of the Monthly Correspondence.

    By then, Ceres had moved too close to the Sun's glare for anyone to verify its position. To recover it, the twenty-four-year-old mathematician Carl Friedrich Gauss devised an efficient orbit-determination method from scratch, predicted where Ceres would reappear, and sent his results to von Zach. On the 31st of December 1801, von Zach and fellow celestial policeman Heinrich W. M. Olbers found the object right where Gauss said it would be. At 2.8 AU from the Sun, Ceres fit the Titius-Bode law almost perfectly. When Neptune was discovered in 1846 eight AU closer to the Sun than the law predicted, most astronomers concluded the law had been a coincidence all along.

  • Piazzi had a specific name in mind: Ceres Ferdinandea. Ceres honored the Roman goddess of agriculture, whose earthly home and oldest temple lay in Sicily, the very island where Piazzi worked. Ferdinandea honored his monarch and patron, King Ferdinand III of Sicily. Other nations rejected the dynastic half of the name, and it was dropped.

    Before von Zach confirmed the object's existence in December 1801, rival names circulated freely. Von Zach himself called it Hera; Bode preferred Juno. Those names gained traction in Germany before the object's reality was fully established. Once it was, astronomers settled on Piazzi's choice, even over his own objections about the dropped suffix.

    The name carried consequences beyond astronomy. Cerium, a rare-earth element discovered in 1803, was named after Ceres shortly after the dwarf planet came to public attention. The old astronomical symbol of Ceres, a sickle, was suggested apparently independently by both von Zach and Bode in 1802. It resembles the symbol for Venus, a circle with a small cross beneath, but with a break in the circle. The generic numbered-disk symbol, which replaced it for asteroid cataloguing purposes, was introduced in 1867, and Ceres entered the new system under the designation 1 Ceres.

  • For more than half a century after its discovery, Ceres appeared in astronomy books as a planet, listed alongside Pallas, Juno, and Vesta. As more objects turned up in the same region, William Herschel introduced the term asteroid, meaning "star-like," for these bodies, writing that they "resemble small stars so much as hardly to be distinguished from them, even by very good telescopes." In 1852 Johann Franz Encke, writing in the Berliner Astronomisches Jahrbuch, declared the old planetary symbols too cumbersome and introduced a numbering system for the new objects in order of discovery.

    Ceres's status wobbled for decades. By the 1860s, a fundamental distinction between major planets and asteroids was widely accepted, yet Ceres sometimes retained a planet-like status because of its geophysical complexity. The debate sharpened dramatically in 2006, when controversy over Pluto forced the International Astronomical Union (IAU) to draft a formal definition of "planet." A proposed definition would have made Ceres the fifth planet from the Sun. On the 24th of August 2006, the IAU assembly instead added the requirement that a planet must have "cleared the neighbourhood around its orbit." Ceres fails that test. It shares its orbit with thousands of other asteroids and accounts for only about forty percent of the asteroid belt's total mass. Bodies that satisfied the first criterion but not the second were placed in the new category of dwarf planets.

    The classification remains contested in practice. Planetary geologists often ignore the IAU definition and treat Ceres as a planet on geophysical grounds. The IAU's own Minor Planet Center notes that dwarf planets may carry dual designations, and the joint IAU/USGS/NASA Gazetteer categorizes Ceres as both an asteroid and a dwarf planet.

  • When the Dawn spacecraft achieved gravitational capture on the 6th of March 2015, it began revealing a world far more active than most scientists had expected. Dawn found Ceres's surface to be a mixture of water, ice, and hydrated minerals including carbonates and clay. On the 9th of December 2015, NASA scientists reported that the striking bright spots scattered across the surface were likely related to a type of salt, specifically a form of brine containing magnesium sulfate hexahydrate. In August 2020, NASA confirmed that Ceres was a water-rich body with a deep reservoir of brine that had percolated to the surface at hundreds of locations.

    The brightest of these spots sit inside the 80 km Occator Crater. The central bright area is named Cerealia Facula, and a cluster of spots to its east is called Vinalia Faculae. Occator contains a pit 9-10 km wide, partially filled by a central dome that post-dates the faculae and is thought to result from the freezing of a subterranean reservoir, comparable in some ways to pingos in Earth's Arctic. A haze that periodically appears above Cerealia supports the idea that outgassing or sublimating ice formed the bright deposits.

    Organic compounds were detected in the Ernutet crater, and at least eleven other regions are candidates for their presence. The near-surface carbon content runs to approximately twenty percent by mass, more than five times higher than in carbonaceous chondrite meteorites studied on Earth. In March 2016, Dawn found definitive evidence of water ice on the surface at Oxo crater. The discovery of ammonium salts in Occator Crater separately supports the idea that Ceres did not form where it now orbits.

  • Ahuna Mons, Ceres's most prominent mountain, stands as the clearest evidence of cryovolcanism on any body this close to the Sun. Its surface shows few impact craters, suggesting a maximum age of 240 million years, young by planetary standards. Its relatively high gravitational field indicates it is dense and composed more of rock than ice. Scientists think its placement results from diapirism, the upward movement of a slurry of brine and silicate particles from the top of the mantle. Ahuna Mons sits roughly antipodal to Kerwan Basin, the largest confirmed crater on Ceres at 284 km across, and seismic energy from the Kerwan-forming impact may have fractured the crust on the opposite side and triggered the flow of high-viscosity cryomagma to the surface.

    A computer simulation published in 2018 suggested that cryovolcanoes on Ceres form and then slowly recede through viscous relaxation over several hundred million years. The team identified twenty-two surface features as strong candidates for relaxed cryovolcanoes. Models indicate that over the past billion years, roughly one cryovolcano has formed every fifty million years, making Ceres the closest known cryovolcanically active body to the Sun.

    Yamor Mons, an older, impact-cratered peak in Ceres's northern polar region, resembles Ahuna Mons despite its greater age because lower polar temperatures slow viscous relaxation there. Hundreds of additional bright spots, or faculae, have been observed across the surface, and an unexpectedly large number of craters contain central pits that may also trace back to cryovolcanic processes. On the 2nd of September 2016, scientists from the Dawn team argued in a Science paper that Ahuna Mons represented the strongest evidence yet for cryovolcanic features on Ceres.

  • Ceres was once thought too small to have retained the heat needed for internal geological activity. Dawn's findings reversed that expectation. Gravity data suggest a partial differentiation into a muddy ice-rock mantle and a crust that is no more than thirty percent ice by volume. In one three-layer model, the outer crust is roughly forty kilometers thick and composed of ice, salts, and hydrated minerals; beneath it lies a sixty-kilometer layer of mixed brine and rock; beneath that sits an inner mantle of hydrated rock such as clays.

    Altogether, scientists estimate Ceres is approximately fifty percent water by volume, compared to just 0.1 percent for Earth, while remaining seventy-three percent rock by mass. The salinity of water leached from rock inside Ceres is estimated at around five percent. Although it lacks tidal heating of the kind that energizes Europa and Enceladus, Ceres is close enough to the Sun and contains enough long-lived radioactive isotopes to preserve liquid water in its subsurface for extended periods.

    Ceres is not as frequently discussed as a candidate for microbial life as Mars, Europa, Enceladus, or Titan are. Yet it possesses carbon, hydrogen, oxygen, and nitrogen, four of the key biochemical elements. Phosphorus has not yet been detected, and sulfur, despite being suggested by earlier Hubble ultraviolet observations, was not confirmed by Dawn. Future missions may settle the question: in 2020, a European Space Agency team proposed the Calathus Mission concept, a sample-return flight targeting the carbonate faculae and dark organics inside Occator Crater, and the China National Space Administration has been designing a sample-return mission from Ceres slated for the 2020s.

Common questions

Who discovered Ceres and when was it found?

Ceres was discovered by Giuseppe Piazzi, a Catholic priest and astronomer, on the 1st of January 1801 at the Palermo Astronomical Observatory in Sicily. Piazzi initially reported it as a comet before recognizing it might be something more significant.

Why was Ceres reclassified from a planet to a dwarf planet?

On the 24th of August 2006, the International Astronomical Union adopted a definition of planet that required a body to have cleared the neighbourhood around its orbit. Ceres fails this criterion because it shares its orbit with thousands of other asteroids and accounts for only about forty percent of the asteroid belt's total mass. Bodies meeting the first but not the second criterion were placed in the new dwarf planet category.

What are the bright spots on Ceres inside Occator Crater?

The bright spots in Occator Crater are deposits of salts left by brines that percolated to the surface. On the 9th of December 2015, NASA scientists identified them as likely involving magnesium sulfate hexahydrate. Near-infrared spectra later confirmed a large amount of sodium carbonate, and in August 2020 NASA confirmed that a deep reservoir of brine had reached the surface at hundreds of locations across Ceres.

What did the Dawn spacecraft find on Ceres?

Dawn, which achieved gravitational capture on the 6th of March 2015, found a surface mixture of water ice, carbonates, and clay minerals. It confirmed cryovolcanic activity centered on Ahuna Mons, detected water ice at Oxo crater in March 2016, and identified organic compounds in the Ernutet crater. The mission ended on the 1st of November 2018 when the spacecraft exhausted its fuel.

Is Ceres a cryovolcanically active body?

Yes. Ceres is the closest known cryovolcanically active body to the Sun. Models indicate that roughly one cryovolcano has formed on average every fifty million years over the past billion years. Ahuna Mons, with a maximum estimated age of 240 million years, is the clearest current example, and a 2018 computer simulation identified twenty-two additional surface features as candidates for relaxed, older cryovolcanoes.

Could Ceres support microbial life?

Ceres has the most water of any body in the inner Solar System after Earth, and brine pockets beneath its surface could provide habitats. Its near-surface carbon content runs to approximately twenty percent by mass, and organic compounds have been detected in the Ernutet crater. Phosphorus has not yet been detected, and unlike Europa or Enceladus, Ceres does not experience tidal heating, though long-lived radioactive isotopes can sustain liquid water in its subsurface.

All sources

158 references cited across the entry

  1. 1bookDictionary of minor planet namesLutz Schmadel — Springer — 2003
  2. 2bookA Journal of Natural Philosophy, Chemistry, and the Arts1802
  3. 3journalThe solar system's invariable planeD. Souami et al. — July 2012
  4. 4webAstDyS-2 Ceres Synthetic Proper Orbital ElementsDepartment of Mathematics, University of Pisa, Italy
  5. 5journalConstraints on Ceres' Internal Structure and Evolution From Its Shape and Gravity Measured by the Dawn SpacecraftA. I. Ermakov et al. — November 2017
  6. 6journalHigh-resolution shape model of Ceres from stereophotoclinometry using Dawn Imaging DataR.S. Park et al. — February 2019
  7. 7journalFaster paleospin and deep-seated uncompensated mass as possible explanations for Ceres' present-day shape and gravityX. Mao et al. — 2018
  8. 8journalThe Ceres gravity field, spin pole, rotation period and orbit from the Dawn radiometric tracking and optical dataA.S. Konopliv et al. — 2018
  9. 9webAsteroid Ceres P_constants (PcK) SPICE kernel fileNASA Navigation and Ancillary Information Facility
  10. 12webLet's Get Serious About CeresBob King — Sky & Telescope — 5 August 2015
  11. 13journalThe Titius-Bode Law and the Discovery of CeresHelen Sawyer Hogg — 1948
  12. 14webCeres: Keeping Well-Guarded Secrets for 215 YearsElizabeth Landau — 26 January 2016
  13. 15webBode's Law and the Discovery of CeresMichael Hoskin — Observatorio Astronomico di Palermo "Giuseppe S. Vaiana" — 26 June 1992
  14. 16journalGauss and the Discovery of CeresEric G. Forbes — 1971
  15. 17bookThe first asteroid: Ceres, 1801–2001Clifford J. Cunningham — Star Lab Press — 2001
  16. 18bookThe Titius-Bode Law of Planetary Distances: Its History and TheoryMichael Martin Nieto — Pergamon Press — 1972
  17. 20bookAsteroids IIIFoderà Serio, G. et al. — University of Arizona Press — 2002
  18. 21bookA Companion to Roman ReligionRüpke, Jörg — John Wiley and Sons — 2011
  19. 23bookThe Dawn Mission to Minor Planets 4 Vesta and 1 CeresA. S. Rivkin — Springer — 2012
  20. 24bookWord For Word From HoraceThornton — Nabu Press — 2012
  21. 25bookFlowers of Roman PoesyBooth — Harvard University — 1823
  22. 26webCerium: historical informationAdaptive Optics
  23. 27webWhat is a Dwarf Planet?JPL/NASA — 22 April 2015
  24. 28bookDiscovery of the First Asteroid, CeresClifford Cunningham — Springer Intl. — 2015
  25. 29journalOn the symbolic notation of the asteroidsB. A. Gould — 1852
  26. 30webWhen Did the Asteroids Become Minor Planets?James L. Hilton — US Naval Observatory — 17 September 2001
  27. 31journalObservations on the two lately discovered celestial BodiesWilliam Herschel — 6 May 1802
  28. 32journalThe Reclassification of Asteroids from Planets to Non-PlanetsPhilip T. Metzger et al. — 2019
  29. 33newsSolar system to welcome three new planetsSteve Connor — 16 August 2006
  30. 34webThe IAU draft definition of "Planet" and "Plutons"Owen Gingerich — IAU — 16 August 2006
  31. 35webThe IAU Draft Definition of Planets and PlutonsSpaceDaily — 16 August 2006
  32. 36journalMasses of the main asteroid belt and the Kuiper belt from the motions of planets and spacecraftE.V. Pitjeva — 2018
  33. 37webIn Depth | Ceres9 November 2017
  34. 40bookThe Cambridge Guide to the Solar SystemKenneth Lang — Cambridge University Press — 2011
  35. 41webQuestion and answers 2International Astronomical Union
  36. 42webEditorial noticeT.B. Spahr — Minor Planet Center (MPC) — 7 September 2006
  37. 43webTarget: CeresInternational Astronomical Union / USGS Astrogeology Science Center / National Aeronautics and Space Administration
  38. 44bookAsteroids IIICellino, A. — University of Arizona Press — 2002
  39. 45journalA Genetic Study of the Ceres (Williams #67) Asteroid FamilyKelley, M. S. et al. — 1996
  40. 46journalCo-orbital objects in the main asteroid beltA. A. Christou — 2000
  41. 47journalA population of Main Belt Asteroids co-orbiting with Ceres and VestaA. A. Christou et al. — January 2012
  42. 48journalDetermination of the mass of Ceres based on the most gravitationally efficient close encountersA. B. Kovačević — 2011
  43. 50journalThe permanently shadowed regions of dwarf planet CeresN. Schorghofer et al. — 6 July 2016
  44. 51web05. Dawn Explores Ceres Results from the Survey OrbitC. T. Russell et al. — NASA — 21 July 2015
  45. 53journalThe surface composition of Ceres from the Dawn missionThomas B. McCord et al. — 15 January 2019
  46. 54webDawn Journal, 28 May 2015Marc D. Rayman — Jet Propulsion Laboratory — 28 May 2015
  47. 55webCeres: The Smallest and Closest Dwarf PlanetNola Taylor Redd — 23 May 2018
  48. 56bookEuropean Planetary Science CongressC. Raymond et al. — September 2018
  49. 58journalThermal evolution of trans-Neptunian objects, icy satellites, and minor icy planets in the early solar systemG.K. Bhatia et al. — 2017
  50. 61journalDawn mission's search for satellites of Ceres: Intact protoplanets don't have satellitesDecember 2018
  51. 63journalNew Constraints on the Abundance and Composition of Organic Matter on CeresHannah H. Kaplan et al. — 21 May 2018
  52. 64journalNew Candidates for Organic-rich Regions on CeresJ. L. Rizos et al. — 2024
  53. 65journalAn aqueously altered carbon-rich CeresS. Marchi et al. — 2018
  54. 66webNew Names and Insights at CeresElizabeth Landau — 28 July 2015
  55. 67journalThe missing large impact craters on CeresS. Marchi et al. — 26 July 2016
  56. 68journalOccator crater in color at highest spatial resolutionA. Nathues et al. — 2019
  57. 69journalCeres and the Terrestrial Planets Impact Cratering RecordR.G. Strom et al. — 2018
  58. 70webHanami Planum on CeresNASA — 23 March 2018
  59. 71journalThe brittle boulders of dwarf planet CeresStefan E Schröder et al. — May 2021
  60. 72journalStagnant lid tectonics: Perspectives from silicate planets, dwarf planets, large moons, and large asteroidsRobert J. Stern et al. — January 2018
  61. 73journalExploring Tectonic Activity on Vesta and CeresD. Buczkowski et al. — December 2017
  62. 74webPIA20348: Ahuna Mons Seen from LAMOJet Propulsion Laboratory — 7 March 2016
  63. 75journalCryovolcanism on CeresO. Ruesch et al. — 2 September 2016
  64. 77journalCryovolcanic rates on Ceres revealed by topographyMichael T. Sori et al. — December 2018
  65. 78journalThe vanishing cryovolcanoes of CeresMichael M. Sori et al. — 2017
  66. 79webCeres takes life an ice volcano at a timeUniversity of Arizona — 17 September 2018
  67. 82webWhat Looks Like Ceres on Earth?Elizabeth Landau et al. — 24 July 2018
  68. 83journalThe central pit and dome at Cerealia Facula bright deposit and floor deposits in Occator Crater, Ceres: Morphology, comparisons and formationPaul Schenk et al. — 1 March 2019
  69. 84webDawn at Ceres: A haze in Occator Crater?Andrew Rivkin — The Planetary Society — 21 July 2015
  70. 86journalPreferential formation of sodium salts from frozen sodium-ammonium-chloride-carbonate brines – Implications for Ceres' bright spotsTuan H. Vu et al. — July 2017
  71. 87journalThe surface composition of Ceres from the Dawn missionThomas B. McCord et al. — 2019
  72. 89journalThe formation and evolution of bright spots on CeresN. T. Stein et al. — 1 March 2019
  73. 91webDawn at Ceres: What Have We Learned?J. C. Castillo Rogez et al. — 2017
  74. 93webPIA22660: Ceres' Internal Structure (Artist's Concept)Jet Propulsion Laboratory — 14 August 2018
  75. 95journalGeochemistry, thermal evolution, and cryovolcanism on Ceres with a muddy ice mantleM. Neveu et al. — 2016
  76. 97journalLocalized sources of water vapour on the dwarf planet (1) CeresM. Küppers et al. — 23 January 2014
  77. 98journalSolar system: Evaporating asteroidH. Campins et al. — 23 January 2014
  78. 99journalEnceladus' Water Vapor PlumeC. J. Hansen et al. — 10 March 2006
  79. 100journalTransient Water Vapor at Europa's South PoleL. Roth et al. — 26 November 2013
  80. 102bookAsteroids IVDavid Jewitt et al. — University of Arizona — 2015
  81. 103bookProtostars and Planets VJewitt, D et al. — University of Arizona Press — 2007
  82. 104journalCeres, a wet planet: The view after DawnThomas B. McCord et al. — May 2022
  83. 105journalCratering on Ceres: Implications for its crust and evolutionH. Hiesinger et al. — 1 September 2016
  84. 106webCeres' geological activity, ice revealed in new researchNASA/Jet Propulsion Laboratory — 1 September 2016
  85. 107journalDawn arrives at Ceres: Exploration of a small, volatile-rich worldC. T. Russell et al. — 2 September 2016
  86. 108journalThe Putative Cerean ExosphereNorbert Schorghofer et al. — 20 November 2017
  87. 109journalLocalized sources of water vapour on the dwarf planet (1) CeresMichael Küppers et al. — January 2014
  88. 111journalThe Surface Composition of CeresAndrew S. Rivkin et al. — 1 December 2011
  89. 112journalWater Group Exospheres and Surface Interactions on the Moon, Mercury, and CeresNorbert Schörghofer et al. — 1 September 2021
  90. 113journalA Sublimation-driven Exospheric Model of CeresL. Tu et al. — 1 December 2014
  91. 114journalThermal stability of ice on Ceres with rough topographyP. O. Hayne et al. — September 2015
  92. 115journalCeres, Vesta, and Pallas: Protoplanets, Not AsteroidsThomas B. McCord et al. — 7 March 2006
  93. 117journalThe Primordial Excitation and Clearing of the Asteroid BeltJean-Marc Petit et al. — 2001
  94. 119webLarge Impact Craters on Ceres Have Gone MissingNancy Atkinson — Universe Today — 26 July 2016
  95. 120journalCeres: Astrobiological Target and Possible Ocean WorldJulie C. Castillo-Rogez et al. — 31 January 2020
  96. 121webNASA's Dawn Mission Spies Ice Volcanoes on CeresMike Wall — 2 September 2016
  97. 122journalCeres: evolution and present stateJ. C. Castillo-Rogez et al. — 2007
  98. 123journalCharacteristics of organic matter on Ceres from VIR/Dawn high spatial resolution spectraM. C. De Sanctis et al. — 17 October 2018
  99. 125bookA Field Guide to the Stars and PlanetsMenzel, Donald H. et al. — Houghton Mifflin — 1983
  100. 126bookThe Observer's Guide to AstronomyPatrick Martinez — Cambridge University Press — 1994
  101. 127journalThe size, shape, density, and albedo of Ceres from its occultation of BD+8°471L. R. Millis et al. — 1987
  102. 128journalAnalysis of the first disk-resolved images of Ceres from ultraviolet observations with the Hubble Space TelescopeJ. W. Parker et al. — 2002
  103. 129webKeck Adaptive Optics Images the Dwarf Planet CeresAdaptive Optics — 11 October 2006
  104. 130journalPhotometric analysis of 1 Ceres and surface mapping from HST observationsJian-Yang Li et al. — 2006
  105. 131newsLargest Asteroid May Be 'Mini Planet' with Water IceHubbleSite — 7 September 2005
  106. 133journalCeres: A Frontier in AstrobiologyJ. M. Houtkooper et al. — 2017
  107. 134journalDawn Mission to Vesta and CeresC. T. Russell et al. — October 2007
  108. 135webNASA's Dawn Captures First Image of Nearing AsteroidCook, Jia-Rui C. et al. — 11 May 2011
  109. 136webYear of the 'Dwarves': Ceres and Pluto Get Their DueP. Schenk — The Planetary Society — 15 January 2015
  110. 137webDawn Journal: Looking Ahead at CeresMarc Rayman — The Planetary Society — 1 December 2014
  111. 138journalDawn Discovery mission to Vesta and Ceres: Present statusC. T. Russel et al. — 2006
  112. 139webDawn Journal: Closing in on CeresMarc Rayman — The Planetary Society — 30 January 2015
  113. 140webDawn Journal: Ceres Orbit Insertion!Marc Rayman — The Planetary Society — 6 March 2015
  114. 141webDawn Journal: Maneuvering Around CeresMarc Rayman — The Planetary Society — 3 March 2014
  115. 142webDawn Journal: Explaining Orbit InsertionMarc Rayman — The Planetary Society — 30 April 2014
  116. 143webDawn Journal: HAMO at CeresMarc Rayman — The Planetary Society — 30 June 2014
  117. 144webDawn Journal: From HAMO to LAMO and BeyondMarc Rayman — The Planetary Society — 31 August 2014
  118. 146webDawn Mission Extended at Ceres19 October 2017
  119. 147journalThe Bright Spots of Ceres Spin Into ViewPhil Plait — 11 May 2015
  120. 148webCeres' Mystery Bright Dots May Have Volcanic OriginIan O'Neill — Discovery Inc. — 25 February 2015
  121. 150webCeres RC3 AnimationJet Propulsion Laboratory — 11 May 2015
  122. 151webNew Clues to Ceres' Bright Spots and OriginsElizabeth Landau — phys.org — 9 December 2015
  123. 152journalBright carbonate deposits as evidence of aqueous alteration on (1) CeresM. C. De Sanctis — 29 June 2016
  124. 153webDawn – Mission StatusMarc Rayman — Jet Propulsion Laboratory — 13 June 2018
  125. 154webDear DawntasmagoriasMarc Rayman — 2018
  126. 156webChina's Deep-space Exploration to 2030Zou, Yongliao et al. — Key Laboratory of Lunar and Deep Space Exploration, National Astronomical Observatories, Chinese Academy of Sciences, Beijing
  127. 157webJPL Small-Body Database Browser: 1 CeresJPL Solar System Dynamics