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. Author manuscript; available in PMC: 2021 Jul 26.
Published in final edited form as: Icarus. 2018 Nov 22;321:346–357. doi: 10.1016/j.icarus.2018.11.008

Figure 3.

Figure 3.

Longitudinal profile of lava in South Kasei Valles based on MOLA DTM. The profile approximates the main lava flow path. Small spikes or apparent uphill sections are due to either post-flow impacts or imperfections in the DTM, such as poorly resolved constrictions.