<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>R. E. Hunter</dc:contributor>
  <dc:creator>D. M. Rubin</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>&lt;div&gt;&lt;div id="12458875" class="article-section-wrapper js-article-section js-content-section  " data-section-parent-id="0"&gt;&lt;p&gt;Craters form when hailstones impact sand. When a hailstone melts, wet but unsaturated sand within the crater is attracted to the hailstone surface by surface tension. Shrinkage of the melting hailstone then produces one or more rings of sand within the impact crater.--Modified journal abstract.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1306/212F8472-2B24-11D7-8648000102C1865D</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>SEPM</dc:publisher>
  <dc:title>Sedimentary structures formed in sand by surface tension on melting hailstones</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>