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Record #152361:

Cordilleran Ice Sheet lobal interactions and glaciotectonic superposition through stadial maxima along a mountain front in south-western British Columbia, Canada / Stephen R. Hicock, Olav B. Lian.

Title: Cordilleran Ice Sheet lobal interactions and glaciotectonic superposition through stadial maxima along a mountain front in south-western British Columbia, Canada / Stephen R. Hicock, Olav B. Lian.
Author(s): Hicock, Stephen R.
Lian, Olav B.
Date: 1999.
In: Boreas. (1999.), Vol. 28(4) (1999)
Abstract: Presents structural, textural and clast data from till exposed in mountain valleys and adjacent piedmont in Fraser Lowland of British Columbia, Canada. Compares subglacial dynamics and flow patterns of late Wisconsinan glaciers to provide information on subglacial behaviour of south-western corner of last Cordilleran ice sheet. Identifies three flow phases. Finds shift in flow directions of valley glaciers. Fraser Lowland piedmont ice may have been part of outlet glacier-ice stream terminating in salt water over continental shelf.
Notes:

Boreas. Vol. 28(4) :531-542 (1999).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.22 -- Glaciers.
551.324.86 -- Glacier streams.
551.33 -- Glacial geology.
551.332 -- Glacial deposition.
551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites.
551.791 -- Pleistocene.
E7 -- Glaciology: glacial geology and ice ages.
(*41) -- Canada.
(*429) -- British Columbia.
SPRI record no.: 152361

MARCXML

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001 SPRI-152361
005 20220929201136.0
007 ta
008 220929s1999####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-152361
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aHicock, Stephen R.
245 10 ‡aCordilleran Ice Sheet lobal interactions and glaciotectonic superposition through stadial maxima along a mountain front in south-western British Columbia, Canada /‡cStephen R. Hicock, Olav B. Lian.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 531-542 :‡bdiags., tables.
500 ## ‡aBoreas. Vol. 28(4) :531-542 (1999).
520 3# ‡aPresents structural, textural and clast data from till exposed in mountain valleys and adjacent piedmont in Fraser Lowland of British Columbia, Canada. Compares subglacial dynamics and flow patterns of late Wisconsinan glaciers to provide information on subglacial behaviour of south-western corner of last Cordilleran ice sheet. Identifies three flow phases. Finds shift in flow directions of valley glaciers. Fraser Lowland piedmont ice may have been part of outlet glacier-ice stream terminating in salt water over continental shelf.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.324.86 -- Glacier streams.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡a551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*429) -- British Columbia.‡2udc
700 1# ‡aLian, Olav B.
773 0# ‡7nnas ‡tBoreas. ‡gVol. 28(4) (1999) ‡wSPRI-56035
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220929