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. 2020 Feb 24;11:1014. doi: 10.1038/s41467-020-14679-1

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© The Author(s) 2020

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 1 — The map shows InSight (NSY) and major physiographic features as well as the landing sites of the Viking Lander 2 (VL2), Mars Science Laboratory (MSL) Curiosity in Gale crater, and the Mars Exploration Rover (MER) Spirit in Gusev crater. InSight landed near the dichotomy boundary between the heavily cratered highlands to the south and the northern lowlands. Volcanic flows from Elysium Mons flowed to the south and very young lavas from Cerberus Fossae flowed down Athabasca Valles to 150 km to the east of the lander. The map is a portion of the MOLA shaded relief topographic map of Mars with elevations with respect to the geoid.