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Record #129706:

Macroforms, large bedforms and rhythmic sedimentary sequences in subglacial eskers, south-central Ontario: implications for esker genesis and meltwater regime / Tracy A. Brennand.

Title: Macroforms, large bedforms and rhythmic sedimentary sequences in subglacial eskers, south-central Ontario: implications for esker genesis and meltwater regime / Tracy A. Brennand.
Author(s): Brennand, Tracy A.
Date: 1994.
Abstract: Considers landform associations, morphology and sedimentology, including clast lithology, sphericity and roundness, of Late Wisconsinan eskers. Four eskers are examined in detail. Large bedforms, macroforms and sedimentary sequences are identified, described and interpreted with respect to esker morphology and meltwater regime responsible for their formation. Attempt is made to relate esker sedimentology systematically to external morphology by invoking formative processes in uniformitarian manner. Model of synchronous subglacial sedimentation for large Pleistocene eskers, where ice-marginal sedimentation was, at most, minor component of esker sedimentation, is presented. Sediment supply and dynamics of glacial hydrologic system are investigated.
Notes:

Offprint: Sedimentary Geology. Vol. 91(1-4) :9-55.

Keywords: 551.33 -- Glacial geology.
551.332.55 -- Ice-contact features.
E7 -- Glaciology: glacial geology and ice ages.
(*41) -- Canada.
(*425) -- Ontario.
Location(s): SCO: SPRI-SHF: 551.332
SPRI record no.: 129706

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100 1# ‡aBrennand, Tracy A.
245 10 ‡aMacroforms, large bedforms and rhythmic sedimentary sequences in subglacial eskers, south-central Ontario :‡bimplications for esker genesis and meltwater regime /‡cTracy A. Brennand.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1994.
300 ## ‡ap. 9-55 :‡bill., diags., tables, maps.
500 ## ‡aOffprint: Sedimentary Geology. Vol. 91(1-4) :9-55.
520 3# ‡aConsiders landform associations, morphology and sedimentology, including clast lithology, sphericity and roundness, of Late Wisconsinan eskers. Four eskers are examined in detail. Large bedforms, macroforms and sedimentary sequences are identified, described and interpreted with respect to esker morphology and meltwater regime responsible for their formation. Attempt is made to relate esker sedimentology systematically to external morphology by invoking formative processes in uniformitarian manner. Model of synchronous subglacial sedimentation for large Pleistocene eskers, where ice-marginal sedimentation was, at most, minor component of esker sedimentation, is presented. Sediment supply and dynamics of glacial hydrologic system are investigated.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.55 -- Ice-contact features.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*425) -- Ontario.‡2udc
852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h551.332‡9Create 1 item record‡0Migrate
917 ## ‡aUnenhanced record from Muscat, imported 2019
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