EPSC Abstracts
Vol. 19, EPSC2026-189, 2026, updated on 02 Jul 2026
https://doi.org/10.5194/epsc2026-189
Europlanet Science Congress 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 10 Sep, 18:00–19:30 (CEST), Display time Thursday, 10 Sep, 08:30–19:30| Foyer 3, F3.76
Colour lithologies of Ceres' south pole
Andreas Nathues1, Maelie Coutelier1, Martin Hoffmann1, Jan Hendrik Pasckert2, Ranjan Sarkar1,3, and Nico Schmedemann2
Andreas Nathues et al.
  • 1Max Planck Institute for Solar System Research, Planets and Comets, Göttingen, Germany (nathues@mps.mpg.de)
  • 2Institut für Planetologie, University of Münster, Germany,
  • 3Indian Institute of Technology, Kharagpur, India

Ceres, the largest object in the main asteroid belt (940 km in diameter), is a survivor of the earliest period of Solar System formation. It orbits the Sun at a mean distance of approximately 2.8 AU. Information about its interior provides essential insights into the formation and evolution of volatile-rich planetary embryos that originated within the protoplanetary disc. From 2015 to 2018, NASA’s Dawn spacecraft collected data in orbit around Ceres [1, 2], returning a wealth of imaging information obtained by the Framing Camera (FC) [3] and the Visible and Infrared Spectrometer (VIR) [4].    

Although the equatorial to mid-latitude regions of Ceres have been extensively mapped and analysed, the polar latitudes (> ±60°) have received comparatively little investigation, primarily due to the suboptimal quality of the returned imaging data, which is a consequence of the challenging illumination conditions. Notably, the south pole was poorly illuminated during the prime mission, a period in which most of the global high-res imaging data were collected.

However, following some improvements in the mosaicking of polar FC imagery in clear (Fig. 1) and colour filters, the analysis of certain sufficiently illuminated surface areas became possible. Contrary to our initial expectations, the south pole region has been found to show a number of distinctive colour lithologies that are also present at lower latitudes. It is noteworthy that the colour of the polar background material often deviates from the global average of Ceres, exhibiting an increased spectral redness. The spectral appearance of the polar lithologies is influenced by this redder background material due to the occurrence of mixing. Also, a dependence on the longitudes of their distribution indicates specific contexts of origin.

Fig. 1: Clear filter mosaic of Ceres' south pole from LAMO orbit (resolution about 35 m/pix.).

[1] Russell, C.T., Raymond, C.A. The Dawn Mission to Vesta and Ceres. Space Sci Rev 163, 3–23 (2011). https://doi.org/10.1007/s11214-011-9836-2

[2] Russell, C.T. et al. Dawn arrives at Ceres: Exploration of a small, volatile-rich world. Science 353, 6303, 1008–1010 (2016). https://doi.org/10.1126/science.aaf4219

[3] Sierks, H. et al. The Dawn Framing Camera in: The Dawn Mission to Minor Planets 4 Vesta and 1 Ceres. Springer, 263–327 (2011). https://link.springer.com/content/pdf/10.1007%2F978-1-4614-4903-4_2.pdf (book)

[4] De Sanctis, M. C. et al. The VIR Spectrometer. Space Sci Rev 163, 329–369 (2011). https://doi.org/10.1007/s11214-010-9668-5

How to cite: Nathues, A., Coutelier, M., Hoffmann, M., Pasckert, J. H., Sarkar, R., and Schmedemann, N.: Colour lithologies of Ceres' south pole, Europlanet Science Congress 2026, The Hague, The Netherlands, 7–11 Sep 2026, EPSC2026-189, https://doi.org/10.5194/epsc2026-189, 2026.