SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #126376:
Snowmelt-induced slushflows, Ellesmere Island, N.W.T., Canada / D.R. Hardy.
Title: | Snowmelt-induced slushflows, Ellesmere Island, N.W.T., Canada / D.R. Hardy. |
Author(s): | Hardy, D. R. |
Date: | [1993] |
In: | Eastern Snow Conference. Proceedings. ([1993]), Vol. 50th Annual Meeting ([1993]) |
Abstract: | Presents analysis of weather and hydrologic activity during May and June 1992, on northern coast, which culminated in rapid movement of water-saturated snow. Sequence of events suggests that slushflows are annual events, originating from partial source areas in high Arctic. |
Notes: | Eastern Snow Conference. Proceedings. Vol. 50th Annual Meeting :423-431 ([1993]). Joint Meeting with 61st Western Snow Conference. |
Keywords: | 551.4 -- Geomorphology. 551.435.627 -- Landslides. 551.311.21 -- Erosion, caused by running water. 551.578.462 -- Snow cover, ablation. E10 -- Glaciology: snow and avalanches. (*41) -- Canada. (*440) -- Northwest Territories. (*460) -- Franklin District. (*464.2) -- Ellesmere Island. |
SPRI record no.: | 126376 |
LDR 01359naa#a2200000#a#4500 001 SPRI-126376 005 20230927122106.0 007 ta 008 230927s1993####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-126376 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHardy, D. R. 245 10 ‡aSnowmelt-induced slushflows, Ellesmere Island, N.W.T., Canada /‡cD.R. Hardy. 260 ## ‡a[S.l.] :‡b[s.n.],‡c[1993] 300 ## ‡ap. 423-431 :‡bdiags. 500 ## ‡aEastern Snow Conference. Proceedings. Vol. 50th Annual Meeting :423-431 ([1993]). 500 ## ‡aJoint Meeting with 61st Western Snow Conference. 520 3# ‡aPresents analysis of weather and hydrologic activity during May and June 1992, on northern coast, which culminated in rapid movement of water-saturated snow. Sequence of events suggests that slushflows are annual events, originating from partial source areas in high Arctic. 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡a551.435.627 -- Landslides.‡2udc 650 07 ‡a551.311.21 -- Erosion, caused by running water.‡2udc 650 07 ‡a551.578.462 -- Snow cover, ablation.‡2udc 650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*440) -- Northwest Territories.‡2udc 651 #7 ‡a(*460) -- Franklin District.‡2udc 651 #7 ‡a(*464.2) -- Ellesmere Island.‡2udc 773 0# ‡7nnas ‡tEastern Snow Conference. Proceedings. ‡gVol. 50th Annual Meeting ([1993]) ‡wSPRI-23848 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230927