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Record #180059:

Supporting evidence from the New York drumlin field that elongate subglacial landforms indicate fast ice flow / Jason P. Briner.

Title: Supporting evidence from the New York drumlin field that elongate subglacial landforms indicate fast ice flow / Jason P. Briner.
Author(s): Briner, Jason P.
Date: 2007.
In: Boreas. (2007.), Vol. 36(2) (2007)
Abstract: Examines drumlins and megaflutes in eastern portion of New York drumlin field to test hypothesis that elongate subglacial landforms indicate fast ice flow. Focuses on measurements of elongation parameters of 548 drumlins between lakes Ontario and Oneida using digital elevation data. Concludes that bedforms, which increase in elongation down flowline, most likely represent zone of fast ice flow during deglaciation of New York and that, since boundaries of swath of elongate bedforms do not coincide with topography, this may signify location of an ice stream.
Notes:

Boreas. Vol. 36(2) :143-147 (2007).

Keywords: 551.33 -- Glacial geology.
551.32 -- Glaciology.
551.324.5 -- Land ice, flow.
551.324.54 -- Land ice, flow of particular glaciers.
551.336 -- Ice ages.
551.324.29 -- Land ice, miscellaneous forms: ice streams.
551.332.5 -- Glacial landforms.
551.332.54 -- Drumlins.
551.324.63 -- Land ice, advance and retreat.
551.791 -- Pleistocene.
E7 -- Glaciology: glacial geology and ice ages.
(74) -- North-eastern states.
SPRI record no.: 180059

MARCXML

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100 1# ‡aBriner, Jason P.
245 10 ‡aSupporting evidence from the New York drumlin field that elongate subglacial landforms indicate fast ice flow /‡cJason P. Briner.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2007.
300 ## ‡ap. 143-147 :‡bill., diags., map.
500 ## ‡aBoreas. Vol. 36(2) :143-147 (2007).
520 3# ‡aExamines drumlins and megaflutes in eastern portion of New York drumlin field to test hypothesis that elongate subglacial landforms indicate fast ice flow. Focuses on measurements of elongation parameters of 548 drumlins between lakes Ontario and Oneida using digital elevation data. Concludes that bedforms, which increase in elongation down flowline, most likely represent zone of fast ice flow during deglaciation of New York and that, since boundaries of swath of elongate bedforms do not coincide with topography, this may signify location of an ice stream.
530 ## ‡aAlso issued online ‡uurn:doi:10.1080/03009480600923394‡uhttps://dx.doi.org/10.1080/03009480600923394
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324.5 -- Land ice, flow.‡2udc
650 07 ‡a551.324.54 -- Land ice, flow of particular glaciers.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.324.29 -- Land ice, miscellaneous forms: ice streams.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.332.54 -- Drumlins.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(74) -- North-eastern states.‡2udc
773 0# ‡7nnas ‡tBoreas. ‡gVol. 36(2) (2007) ‡wSPRI-56035
916 ## ‡a2007/07/23 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221004 ‡bRF