boulders beyond the Ross I and Alpine I drift limits but within the Taylor III drift limit of Denton et al, figure 3) are grussified, cavernously weathered, and wind faceted. Stones on moraines above (and thus old - Alpine Valleys - Document - PDFSEARCH.IO

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	boulders beyond the Ross I and Alpine I drift limits but within the Taylor III drift limit of Denton et al, figure 3) are grussified, cavernously weathered, and wind faceted. Stones on moraines above (and thus old Add to Reading List Document Date: 2011-05-06 05:15:43 Open Document File Size: 3,78 MB Share Result on Facebook

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boulders beyond the Ross I and Alpine I drift limits but within the Taylor III drift limit of Denton et al, figure 3) are grussified, cavernously weathered, and wind faceted. Stones on moraines above (and thus oldAdd to Reading List