The Cassini mission discovered lakes and seas comprising mostly methane in the polar regions of Titan. Lakes of liquid nitrogen may have existed during the epochs of Titan’s past in which methane was photochemically depleted, leaving a nearly pure molecular nitrogen atmosphere and, thus, far colder temperatures. The modern-day small lake basins with sharp edges have been suggested to originate from dissolution processes, due to their morphological similarity to terrestrial karstic lakes. Here we analyse the morphology of the small lake basins that feature raised rims to elucidate their origin, using delay-Doppler processed altimetric and bathymetric data acquired during the last close flyby of Titan by the Cassini spacecraft. We find that the morphology of the raised-rim basins is analogous to that of explosion craters from magma–water interaction on Earth and therefore propose that these basins are from near-surface vapour explosions, rather than karstic. We calculate that the phase transition of liquid nitrogen in the near subsurface during a warming event can generate explosions sufficient to form the basins. Hence, we suggest that raised-rim basins are evidence for one or more warming events terminating a nitrogen-dominated cold episode on Titan.
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The authors declare that the data supporting the findings of this study are available within the article and its supplementary information.
The mathematical algorithms that support findings of this study are available from the corresponding author upon request.
Stofan, E. R. et al. The lakes of Titan. Nature 445, 61–64 (2007).
Lopes, R. M. et al. The lakes and seas of Titan. EOS Trans. Am. Geophys. Union 88, 569–570 (2007).
Hayes, A. et al. Hydrocarbon lakes on Titan: distribution and interaction with a porous regolith. Geophys. Res. Lett. 35, L09204 (2008).
Aharonson, O. et al. An asymmetric distribution of lakes on Titan as a possible consequence of orbital forcing. Nat. Geosci. 2, 851–854 (2009).
Hayes, A. G. et al. Transient surface liquid in Titan’s polar regions from Cassini. Icarus 211, 655–671 (2011).
Mastrogiuseppe, M. et al. The bathymetry of a Titan sea. Geophys. Res. Lett. 41, 1432–1437 (2014).
Mastrogiuseppe, M. et al. Deep and methane-rich lakes on Titan. Nat. Astron. 3, 535–542 (2019).
Yung, Y. L., Allen, M. & Pinto, J. P. Photochemistry of the atmosphere of Titan: comparison between model and observations. Astrophys. J. Suppl. Ser. 55, 465–506 (1984).
Hayes, A. G. et al. Topographic constraints on the evolution and connectivity of Titan’s lacustrine basins. Geophy. Res. Lett. 44, 11745–11753 (2017).
Poggiali, V. et al. High-resolution topography of Titan adapting the delay/Doppler algorithm to the Cassini RADAR altimeter data. IEEE Trans. Geosci. Remote Sens. https://doi.org/10.1109/TGRS.2019.2912575 (2019).
Hayes, A. G. The lakes and seas of Titan. Annu. Rev. Earth Planet. Sci. 44, 57–83 (2016).
Birch, S. P. D. et al. Geomorphologic mapping of Titan’s polar terrains: constraining surface processes and landscape evolution. Icarus 282, 214–236 (2017).
Birch, S. P. D. et al. Raised rims around Titan’s sharp-edged depressions. Geophys. Res. Lett. 46, 5846–5854 (2018).
Malaska, M. et al. Identification of karst-like terrain on Titan from valley analysis. In Proc. 41st Lunar Planet. Sci. Conf. 1544 (USRA, 2010).
Cornet, T. et al. Dissolution on Titan and on Earth: toward the age of Titan’s karstic landscapes. J. Geophys. Res. Planets 120, 1044–1074 (2015).
Perron, J. T. et al. Valley formation and methane precipitation rates on Titan. J. Geophys. Res. Planets 111, E11001 (2006).
Krasnopolsky, V. A. A photochemical model of Titan’s atmosphere and ionosphere. Icarus 201, 226–256 (2009).
Lorenz, R. D., McKay, C. P. & Lunine, J. I. Photochemically-driven collapse of Titan’s atmosphere. Science 275, 642–644 (1997).
Lorenz, V. Maar-diatreme volcanoes, their formation, and their setting in hard-rock or soft-rock environments. Geolines 15, 72–83 (2003).
Graettinger, A. H. Trends in maar crater size and shape using the global Maar Volcano Location and Shape (MaarVLS) database. J. Volcanol. Geotherm. Res. 357, 1–13 (2018).
Valentine, G. A. et al. Experiments with vertically- and laterally-migrating subsurface explosions with applications to the geology of phreatomagmatic and hydrothermal explosion craters and diatremes. Bull. Volcanol. 77, 15 (2015).
Begét, J. E., Hopkins, D. M. & Charron, S. D. The largest known maars on Earth, Seward Peninsula, northwest Alaska. Arctic 49, 62–69 (1996).
Avellán, D. R., Macías, J. L., Pardo, N., Scolamacchia, T. & Rodriguez, D. Stratigraphy, geomorphology, geochemistry and hazard implications of the Nejapa Volcanic Field, western Managua, Nicaragua. J. Volcanol. Geotherm. Res. 213-214, 51–71 (2012).
Valentine, G. A., Graettinger, A. H. & Sonder, I. Explosion depths for phreatomagmatic eruptions. Geophys. Res. Lett. 41, 3045–3051 (2014).
Ross, P.-S. et al. Experimental birth of a maar-diatreme volcano. J. Volcanol. Geotherm. Res. 260, 1–12 (2013).
Seib, N., Kley, J. & Büchel, G. Identification of maars and similar volcanic landforms in the West Eifel Volcanic Field through image processing of DTM data: efficiency of different methods depending on preservation state. Int. J. Earth Sci. 102, 875–901 (2013).
White, J. D. L. Pliocene subaqueous fans and Gilbert-type deltas in maar crater lakes, Hopi Buttes, Navajo Nation (Arizona), USA. Sedimentology 39, 931–946 (1992).
Black, B. A., Perron, J. T., Burr, D. M. & Drummond, S. A. Estimating erosional exhumation on Titan from drainage network morphology. J. Geophys. Res. Planets 117, E08006 (2012).
Charnay, B., Forget, F., Tobie, G., Sotin, C. & Wordsworth, R. Titan’s past and future: 3D modeling of a pure nitrogen atmosphere and geological implications. Icarus 241, 269–279 (2014).
Valentine, G. A. et al. Tephra ring interpretation in light of evolving maar-diatreme concepts: Stracciacappa maar (central Italy). J. Volcanol. Geotherm. Res. 308, 19–29 (2015).
Solomonidou, A. et al. Spectral and emissivity analysis of the raised ramparts around Titan’s northern lakes. Icarus https://doi.org/10.1016/j.icarus.2019.05.040 (2019).
Michaelides, R. J. et al. Constraining the physical properties of Titan’s empty lake basins using nadir and off-nadir Cassini RADAR backscatter. Icarus 270, 57–66 (2016).
Tchamabé, B. C. et al. Towards the reconstruction of the shallow plumbing system of the Barombi Mbo Maar (Cameroon) implications for diatreme growth processes of a polygenetic maar volcano. J. Volcanol. Geotherm. Res. 301, 293–313 (2015).
Hörst, S. M. Titan’s atmosphere and climate. J. Geophys. Res. Planets 122, 432–482 (2017).
Tobie, G., Lunine, J. I. & Sotin, C. Episodic outgassing as the origin of atmospheric methane on Titan. Nature 440, 61–64 (2006).
Smith, B. A. et al. Voyager 2 at Neptune: imaging science results. Science 246, 1422–1449 (1989).
Soderblom, L. A. et al. Triton’s geyser-like plumes: discovery and basic characterization. Science 250, 410–415 (1990).
Duxbury, N. S. & Brown, R. H. The role of an internal heat source for the eruptive plumes on Triton. Icarus 125, 83–93 (1997).
Elliot, J. Letal Global warming on Triton. Nature 393, 765–767 (1998).
Buratti, B. J., Hicks, M. D. & Newburn, R. L. Jr Does global warming make Triton blush? Nature 397, 219 (1999).
Hicks, M. D. & Buratti, B. J. The spectral variability of Triton from 1997–2000. Icarus 171, 210–218 (2004).
Sloan, E. D. & Koh, C. Clathrate Hydrates of Natural Gases 3rd edn (CRC, 2008).
Holsapple, K. A. & Schmidt, R. M. On the scaling of crater dimensions: 1. Explosive processes. J. Geophys. Res. Solid Earth 85, 7247–7256 (1980).
Goto, A., Taniguchi, H., Yoshida, M., Ohba, T. & Oshima, H. Effects of explosion energy and depth to the formation of blast wave and crater: field explosion experiment for the understanding of volcanic explosion. Geophys. Res. Lett. 28, 4287–4290 (2001).
Valentine, G. A. et al. Experimental craters formed by single and multiple buried explosions and implications for volcanic craters with emphasis on maars. Geophys. Res. Lett. 39, L20301 (2012).
Kehle, R. O. Deformation of the Ross Ice Shelf, Antarctica. Geol. Soc. Am. Bull. 75, 259–286 (1964).
Litwin, K. L., Zygielbaum, B. R., Polito, P. J., Sklar, L. S. & Collins, G. C. Influence of temperature, composition, and grain size on the tensile failure of water ice: implications for erosion on Titan. J. Geophys. Res. Planets 117, E08013 (2012).
Graettinger, A. H. et al. Maar-diatreme geometry and deposits: subsurface blast experiments with variable explosion depth. Geochem. Geophys. Geosyst. 15, 740–764 (2014).
The authors thank A. H. Graettinger and J. Radebaugh for useful comments. We thank A. Hayes for his constructive comments on the manuscript. G.M. expresses appreciation to A. Solomonidou for sharing her results. J.I.L. acknowledges support from the Cassini project, subcontract 1437803. V.P. acknowledges funding for this work from the NASA PDART programme grant number 80NSSC18K0513.
The authors declare no competing interests.
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Mitri, G., Lunine, J.I., Mastrogiuseppe, M. et al. Possible explosion crater origin of small lake basins with raised rims on Titan. Nat. Geosci. 12, 791–796 (2019). https://doi.org/10.1038/s41561-019-0429-0