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Recurring slope lineae have been observed on its central-peak slopes, as have relatively youthful gully-like landforms; the latter are observed adjacent to or in the midst of the former, as well as on all of the rim-material slopes. Three of the gullied slopes on the northern-rim materials exhibit landscape features that, on Earth, are synonymous with\n                    <jats:italic toggle=\"yes\">wet<\/jats:italic>\n                    periglaciation, i.e. landscape modification by the freeze\u2013thaw cycling of water. These features include: (1) gelifluction-like lobes; (2) patches of surface polygonization, possibly underlain by ice wedges and formed by thermal-contraction cracking; and (3) shallow, rimless and polygonized basins morphologically akin to terrestrial alases. Here, we use the spatial association of the gully-like landforms together with the putatively\n                    <jats:italic toggle=\"yes\">wet<\/jats:italic>\n                    periglacial assemblages or complexes to deduce and ascribe, albeit indirectly, a wet origin to the former.\n                  <\/jats:p>","DOI":"10.1144\/sp467.7","type":"journal-article","created":{"date-parts":[[2018,3,6]],"date-time":"2018-03-06T20:10:29Z","timestamp":1520367029000},"page":"211-231","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":3,"title":["Periglacial complexes and the deductive evidence of \u2018wet\u2019-flows at the Hale impact crater, Mars"],"prefix":"10.1144","volume":"467","author":[{"given":"R. J.","family":"Soare","sequence":"first","affiliation":[{"name":"Department of Geography, Dawson College, Montreal, Canada H3Z 1A4"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"S. 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M.","family":"Dohm","sequence":"additional","affiliation":[{"name":"Foundation for Advancement of International Science, 24-16, Kasuga, 3-chome, Tsukuba, Ibaraki 305-0821, Japan"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"D.","family":"Reiss","sequence":"additional","affiliation":[{"name":"Institut f\u00fcr Planetologie, Westf\u00e4lische Wilhelms-Universit\u00e4t, M\u00fcnster, Germany 48149"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1881","published-online":{"date-parts":[[2018,3,6]]},"reference":[{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1002\/ppp.622"},{"key":"e_1_3_2_3_1","doi-asserted-by":"publisher","DOI":"10.1002\/grl.50586"},{"key":"e_1_3_2_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.pss.2012.10.008"},{"key":"e_1_3_2_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2009.05.031"},{"key":"e_1_3_2_6_1","first-page":"123","article-title":"Polygonal patterns and ground conditions from aerial photographs","volume":"18","author":"Black R.F.","year":"1952","unstructured":"BlackR.F. 1952. 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