https://wiki.pathfindersonline.org/index.php?action=history&feed=atom&title=Translations%3AAdventist_Youth_Honors_Answer_Book%2FNature%2FGeology%2F14%2FenTranslations:Adventist Youth Honors Answer Book/Nature/Geology/14/en - Revision history2026-04-27T00:35:20ZRevision history for this page on the wikiMediaWiki 1.35.5https://wiki.pathfindersonline.org/index.php?title=Translations:Adventist_Youth_Honors_Answer_Book/Nature/Geology/14/en&diff=307907&oldid=prevFuzzyBot: Importing a new version from external source2021-01-07T23:27:07Z<p>Importing a new version from external source</p>
<p><b>New page</b></p><div>At the 'start' of a classic valley glacier is the cirque, which has a bowl shape with escarped walls on three sides, but open on the side that descends into the valley. In the cirque, an accumulation of ice is formed. These begin as irregularities on the side of the mountain, which are later augmented in size by the coining of the ice. After the glacier melts, these corries are usually occupied by small mountain lakes called tarns.</div>FuzzyBot