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<h2 id="see-also">See also</h2> <ul><li><a href="/facts/Concentric_crater_fill/KVF2fhUn">Concentric crater fill</a> – Landform where the floor of a crater is mostly covered by parallel ridges</li> <li><a href="/facts/Glacier/8GrKVUSS">Glacier</a> – Persistent body of ice that moves downhill under its own weight</li> <li><a href="/facts/Glaciers_on_Mars/CEYMmdT6">Glaciers on Mars</a> – Extraterrestrial bodies of ice</li> <li><a href="/facts/Ismenius_Lacus_quadrangle/3vveemVl">Ismenius Lacus quadrangle</a> – Map of Mars</li> <li><a href="/facts/Lineated_valley_fill/GxV8f7WR">Lineated valley fill</a> – Martian geologic feature</li> <li><a href="/facts/Lobate_debris_apron/qub4Yo3C">Lobate debris apron</a> – Geological features on Mars</li> <li><a href="/facts/Martian_dichotomy/11Ixk04I">Martian dichotomy</a> – Geomorphological feature of Mars</li> <li><a href="/facts/Nilosyrtis_Mensae/hvJFAW2r">Nilosyrtis Mensae</a> – Fretted terrain in the Casius quadrangle on Mars</li> <li><a href="/facts/Protonilus_Mensae/oIk97s4s">Protonilus Mensae</a> – Martian plain</li> <li><a href="/facts/Upper_Plains_Unit/HrKcuH6m">Upper Plains Unit</a> – Surface features of MarsPages displaying short descriptions of redirect targets</li></ul> <h2 id="references">References</h2> <ol> <li id="fn:1"><p>Levy, J., J. Head, D. Marchant. 2009. Concentric crater fill in Utopia Planitia: History and interaction between glacial “brain terrain” and periglacial mantle processes. Icarus 202, 462–476. <a href="#fnref:1" class="footnote-back-ref">↩</a></p></li> <li id="fn:2"><p>Levy, J., J. Head, D. Marchant. 2009. Concentric crater fill in Utopia Planitia: History and interaction between glacial “brain terrain” and periglacial mantle processes. Icarus 202, 462–476. <a href="#fnref:2" class="footnote-back-ref">↩</a></p></li> <li id="fn:3"><p>Baker, D., J. Head. 2015. Extensive Middle Amazonian mantling of debris aprons and plains in Deuteronilus Mensae, Mars: Implication for the record of mid-latitude glaciation. Icarus: 260, 269-288. <a href="#fnref:3" class="footnote-back-ref">↩</a></p></li> <li id="fn:4"><p>Souness, C. and B. Hubbard. 2013. An alternative interpretation of late Amazonian ice flow: Protonilus Mensae, Mars. Icarus 225, 495-505. <a href="#fnref:4" class="footnote-back-ref">↩</a></p></li> <li id="fn:5"><p>Barlow, N. 2008. Mars: An Introduction to its Interior, Surface and Atmosphere. Cambridge University Press. ISBN 978-0-521-85226-5 <a href="/wiki/ISBN_(identifier)" target="_blank">/wiki/ISBN_(identifier)</a> <a href="#fnref:5" class="footnote-back-ref">↩</a></p></li> <li id="fn:6"><p>Head, J. and D. Marchant. 2006. Evidence for global-scale northern mid-latitude glaciation in the Amazonian period of Mars: Debris-covered glacial and valley glacial deposits in the 30 - 50 N latitude band. Lunar. Planet. Sci. 37. Abstract 1127 <a href="#fnref:6" class="footnote-back-ref">↩</a></p></li> <li id="fn:7"><p>Head, J. and D. Marchant. 2006. Modifications of the walls of a Noachian crater in Northern Arabia Terra (24 E, 39 N) during northern mid-latitude Amazonian glacial epochs on Mars: Nature and evolution of Lobate Debris Aprons and their relationships to lineated valley fill and glacial systems. Lunar. Planet. Sci. 37. Abstract 1128 <a href="#fnref:7" class="footnote-back-ref">↩</a></p></li> <li id="fn:8"><p>Head, J., et al. 2006. Extensive valley glacier deposits in the northern mid-latitudes of Mars: Evidence for the late Amazonian obliquity-driven climate change. Earth Planet. Sci. Lett. 241. 663-671 <a href="#fnref:8" class="footnote-back-ref">↩</a></p></li> <li id="fn:9"><p>Head, J., et al. 2006. Modification if the dichotomy boundary on Mars by Amazonian mid-latitude regional glaciation. Geophys. Res Lett. 33 <a href="#fnref:9" class="footnote-back-ref">↩</a></p></li> </ol>