Amazonis Planitia is a broad plain on Mars, covered with ancient lava. This image shows an interesting feature of an old lava flow.
<p>When it was mostly liquid, the lava had a crust of cooled debris floating on the surface. Here, the crust just barely scraped over some hills. The flow was able to make it past the hills, but the rubble crust was caught and piled up, forming thick masses of debris.
</p><p><a rel="nofollow" class="external text" href="http://static.uahirise.org/images/2017/details/cut/ESP_048745_2095.jpg">Downstream from the hills</a>, there was no crust left and the lava formed a smoother, fresh surface. Observations like this tell us about the scale of the lava flow (which must have been a huge sheet) and also which direction it was moving at the time when the crust interacted with the hills.
</p><p>The map is projected here at a scale of 50 centimeters (19.7 inches) per pixel. [The original image scale is 59.0 centimeters (23.2 inches) per pixel (with 2 x 2 binning); objects on the order of 177 centimeters (69.7 inches) across are resolved.] North is up.
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The University of Arizona, Tucson, operates HiRISE, which was built by Ball Aerospace &amp; Technologies Corp., Boulder, Colo. NASA's Jet Propulsion Laboratory, a division of Caltech in Pasadena, California, manages the Mars Reconnaissance Orbiter Project for NASA's Science Mission Directorate, Washington.
NASA/JPL-Caltech/Univ. of Arizona
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