Volcanoes on Mars (composite catalog)

Shapefile https://www.dropbox.com/s/554yilypb5sx0cs/volcano.zip?dl=0
Notes All data were re-drawn as ellipses that best fit the feature in THEMIS Day imagery and/or MOLA relief. All values were calculated from the re-drawn ellipses.
Lat/Lon are calculated as the centers of ellipses, not Lat/Lon values in the source papers
Diameter, area, perimeter are calculated from the ellipses, and are not taken from the source papers. Diameter is an average, calculated from perimeter.
Height (Max. elev, range of elevation) data are calculated from within the ellipses, and are not taken from the source papers. Heigh data is from MOLA gridded data. MAX=max elevation point within the ellipse, MIN: min. elevation value point within the ellipse
Type/interpretations are taken from the source papers. For small cones and mounds, interpretations vary (pingo/volcano/mud volcano). All features that have at least one volcanic interpretation in a recent (ca. last two decades) paper are included. Features previously (Viking) identified as volcanic but recently reclassified are not included.

Confidence. Major and minor shields, calderas, fissure/small/low shields and lava domes can be considered as confirmed, while all others are candidate volcanic features.

Group: a single ellipse is one example showing actual size, which is part of a group of similar sized features. These are typically interpreted as pseudocraters (rootless cones) or pingos or mud volcanoes.
Type: Caldera: size/range values represent caldera, not volcanic construct (if any). These are caldera volcanoes without substantial construct. (negative relief forms)
Database Editor Henrik Hargitai, with the help of P. Broz



  • Baptista, A. R., N. Mangold, V. Ansan, D. Baratoux, P. Lognonne´, E. I. Alves, D. A. Williams, J. E. Bleacher, P. Masson, and G. Neukum (2008), A swarm of small shield volcanoes on Syria Planum, Mars,J. Geophys. Res., 113, E09010, doi:10.1029/2007JE002945.
  • Baratoux D, Pinet P, Toplis MJ, Mangold N, Greeley R, Baptista AR (2009) Shape, rheology and emplacement times of small Martian shield volcanoes. J Volcanol Geotherm Res 185:47–68
  • Bleacher JE, Greeley R, Williams DA, Cave SR, Neukum G (2007) Trends in effusive style at the Tharsis Montes, Mars, and implications for the development of the Tharsis province. J Geophys Res 112:E09005. doi:10.1029/2006JE002873
  • Broz P, Hauber E (2012) Amenthes cones, Mars: hydrovolcanic (tuff) cones from phreatomagmatic explosive eruptions? 43rd Lunar Planet Sci Conf, abstract #1321, Houston
  • Brož, P., and E. Hauber (2013), Hydrovolcanic tuff rings and cones as indicators for phreatomagmatic explosive eruptions on Mars, J. Geophys. Res. Planets, 118, 1656–1675, doi:10.1002/jgre.20120.
  • Brož, P., Hauber, E., Platz, T., Balme, M., (2015b). Evidence for Amazonian highly viscous lavas in southern highlands on Mars, Earth and Planetary Science Letters, 415, 200–212, doi: 10.1016/j.epsl.2015.01.033.
  • Brož, P., O. Čadek, E. Hauber, and A. P. Rossi (2015), Scoria cones on Mars: Detailed investigation of morphometry based on high-resolution digital elevation models, J. Geophys. Res. Planets, 120, 1512–1527, doi:10.1002/2015JE004873.
  • Bruno BC, Fagents SA, Hamilton CW, Burr DM, Baloga SM (2006) Identification of volcanic rootless cones, ice mounds, and impact craters on Earth and Mars: using spatial distribution as a remote sensing tool. J Geophys Res 111:E06017. doi:10.1029/2005JE002510
  • Fagan, A.L., Sakimoto, S.E.H., Hughes, S.S., 2010. Formation constraints on Matian north polar volcanic edifeces. J. Geophys. Res. 115, E07013, doi:10.1029/2009JE003476
  • Ghatan, G.J., Head, J.W., 2002. Candidate subglacial volcanoes in the south polar region of Mars: Morphology, morphometry, and eruption conditions. J. Geophys. Res 107, 1-21
  • Ghent RR, Anderson SW, Pithawala TM (2012) The formation of small cones in Isidis Planitia, Mars through mobilization of pyroclastic surge deposits. Icarus 217:169–183
  • Harrison,  K.  P,  Chapman,  M.  G.,  2008.  Evidence  for ponding  and  catastrophic  floods  in  central  Valles  Marineris,  Mars, Icarus,198, 351–364, doi: 10.1016/j.icarus.2008.08.003
  • Hauber E, Bleacher J, Gwinner K, Williams D, Greeley R (2009) The topography and morphology of low shields and associated landforms of plains volcanism in the Tharsis region of Mars. J Volcanol Geotherm Res 185:69–95
  • Hodges CA, Moore HJ (1984) Atlas of Volcanic Landforms on Mars. USGS Prof. Paper 1534
  • Hovius, N., Lea-Cox, A., Turowski, J.M., 2008. Recent volcano-ice interaction and outburst flooding in a Mars polar cap re-entrant. Icarus 197:24–38.
  • Keszthelyi, L., W. Jaeger, A. McEwen, L. Tornabene, R. A. Beyer, C. Dundas, and M. Milazzo (2008), High Resolution Imaging Science Experiment (HiRISE) images of volcanic terrains from the first 6 months of the Mars Reconnaissance Orbiter Primary Science Phase,J. Geophys. Res., 113, E04005, doi:10.1029/2007JE002968.
  • Keszthelyi LP, Jaeger WL, Dundas CM, Marti´nezAlonso S, McEwen AS, Milazzo MP (2010) Hydrovolcanic features on Mars: preliminary observations from the first Mars year of HiRISE imaging. Icarus 205(1):211–229
  • Lanagan PD, McEwen AS, Keszthelyi LP, Thordarson T (2001) Rootless cones on Mars indicating the presence of shallow equatorial ground ice in recent times. Geophys Res Lett 28(12):2365–236
  • Martínez-Alonso, S., Mellon, M. T., Banks, M.E., Keszthelyi, L. P., McEwen, A. S., The HiRISE Team, 2011. Evidence of volcanic     and     glacial     activity     in     Chryse     and     Acidalia     Planitiae,     Mars,     Icarus,212,     597–621, doi:10.1016/j.icarus.2011.01.004.
  • Meresse S, Costard F, Mangold N, Masson P and the HRSC Team (2008) Formation and evolution of the chaotic terrains by subsidence and magmatism: Hydraotes Chaos, Mars. Icarus 194, 487–500
  • Michalski JR, Bleacher JE (2013) Supervolcanoes within an ancient
    volcanic province in Arabia Terra, Mars. Nature 502, doi:10.1038/nature12482
  • Mouginis-Mark, P. J., and P. R. Christensen (2005), New observations of volcanic features on Mars from the THEMIS instrument, J. Geophys. Res., 110, E08007, doi:10.1029/2005JE002421.
  • Pajola M et al. 2016. The Simud–Tiu Valles hydrologic system: A multidisciplinary study of a possible site for future Mars on-site exploration. Icarus 268, 355–381
  • Plescia, J. B. 1990. Recent flood lavas in the Elysium region of Mars. Icarus 88, 465–490
  • Platz,  T.,  Michael,  G.G.,  2011.  Eruption  history  of  the  Elysium  Volcanic  Province, Mars.  Earth  and  Planetary  Science Letters,312, 140–151, doi:10.1016/j.epsl.2011.10.001
  • Plescia, J. B. (2004), Morphometric properties of Martian volcanoes,J. Geophys. Res., 109, E03003, doi:10.1029/2002JE002031
  • Rampey, M. L., K. A. Milam, H. Y. McSween Jr., J. E. Moersch, and P. R. Christensen (2007), Identity and emplacement of domical structures in the western Arcadia Planitia, Mars, J. Geophys. Res., 112, E06011, doi:10.1029/2006JE002750.
  • Robbins SJ, Di Achille G, Hynek BM (2011) The volcanic history of Mars: high resolution crater-based studies of the calderas of 20 volcanoes. Icarus 211:1179–1203. doi:10.1016/j.icarus.2010.11.012
  • Skinner JA, Tanaka KL (2007) Evidence for and implications of sedimentary diapirism and mud volcanism in the southern Utopia highland–lowland boundary plain, Mars. Icarus 186, 41–5
  • Stewart EM, Head JW (2001) Ancient Martian vcanies in the Aeolis region: new evidence from MOLA data. JGR 106 17505-17513
  • Tanaka, K.L., Skinner, J.A., Jr., Dohm, J.M., Irwin, R.P., III, Kolb, E.J., Fortezzo, C.M., Platz, T., Michael, G.G., and Hare, T.M., 2014, Geologic map of Mars: U.S. Geological Survey Scientific Investigations Map 3292, scale 1:20,000,000, pamphlet 43 p., http://dx.doi.org/10.3133/sim3292.
  • Vaucher J, Baratoux D, Mangold N, Pinet P, Kurita K, Gre´goire M (2009) The volcanic history of central Elysium Planitia: implications for martian magmatism. Icarus 204:418–442
  • Williams DA et al. (2011) The Circum-Hellas Volcanic Province, Mars: Overview. Planetary and Space Science 57 (2009) 895–916
  • Xiao L, Huang J, Christensen PR, Greeley R, Williams DA, Zhao J, He Q (2012) Ancient volcanism and its implication for thermal evolution of Mars. Earth and Planetary Science Letters 323–324, 9–18