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Showing 1 to 2 of 2 for “"Diversion channel"”.
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The geology of eastern Wells County, North Dakota
… directional features and superimposed meltwater channels. A major stillstand of this phase formed the Martin end moraine to the northwest of the area.</p> <p>The essentially contemporaneous Leeds lobs advanced from the north-northeast. The Heimdal end moraine was formed during a major stillstand …