Crystal orientation in glacier and in experimentally deformed ice / George P. Rigsby.

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035 ## ‡aSPRI-33944
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100 1# ‡aRigsby, George P.
245 10 ‡aCrystal orientation in glacier and in experimentally deformed ice /‡cGeorge P. Rigsby.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1960.
300 ## ‡ap. 589-606, [4] unnumbered leaves (folded) :‡bill., diags., maps.
500 ## ‡aJournal of Glaciology. Vol. 3(27) :589-606, [4] unnumbered leaves (folded) (1960).
520 3# ‡aOver 8000 ice crystals were oriented and measured for crystal-fabric studies from temperate and polar glaciers, using large universal stage and thin-section techniques. Very strong fabrics have been found and laboratory experiments were carried out to investigate problems of glacier flow. Concludes that proper orientation of crystal in order to glide on basal plane is important in flow of polar glacier ice, and that gliding plus recrystallization or continual boundary migration is important in flow of temperate glacier ice.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.324.51 -- Land ice, theory of flow.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a548.5 -- Ice crystals.‡2udc
773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 3(27) (1960) ‡wSPRI-20534
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230331