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Record #180059:
- #180059
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MARC recordSupporting 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 |
LDR 01876naa#a2200000#a#4500 001 SPRI-180059 005 20231005043833.0 007 ta 008 231005s2007####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-180059 040 ## ‡aUkCU-P‡beng‡eaacr 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# ‡a20231005 ‡bRF