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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #140227:
Evolution of marginal zones during glacial retreat in NW Wedel Jarlsberg Land, Spitsbergen / Jan Reder.
Title: | Evolution of marginal zones during glacial retreat in NW Wedel Jarlsberg Land, Spitsbergen / Jan Reder. |
Author(s): | Reder, Jan. |
Date: | 1996. |
In: | Polish Polar Research. (1996.), Vol. 17(1-2) (1996) |
Abstract: | Complex analysis of geomorphological glacial processes in forefields of retreating glaciers was undertaken. Field studies and archival cartographic materials indicate continued glacial retreat, at least since turn of century. Average rate is now 20 m/yr, with no moraine ridges formed, except for fluted moraines. At present glaciofluvial erosion predominates. |
Notes: | Polish Polar Research. Vol. 17(1-2) :61-84, 4 plates (at end) (1996). |
Keywords: | 551.324 -- Land ice. 551.324.63 -- Land ice, advance and retreat. 551.331 -- Glacial erosion. 551.332.58 -- Outwash plains. 556.51 -- River basins and watersheds. E7 -- Glaciology: glacial geology and ice ages. (*3) -- Arctic regions. (*32) -- Svalbard. |
SPRI record no.: | 140227 |
LDR 01350naa#a2200000#a#4500 001 SPRI-140227 005 20231003022242.0 007 ta 008 231003s1996####xx#abf|##|###|0||#0|eng#d 035 ## ‡aSPRI-140227 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aReder, Jan. 245 10 ‡aEvolution of marginal zones during glacial retreat in NW Wedel Jarlsberg Land, Spitsbergen /‡cJan Reder. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1996. 300 ## ‡ap. 61-84, 4 plates (at end) :‡bdiag., maps. 500 ## ‡aPolish Polar Research. Vol. 17(1-2) :61-84, 4 plates (at end) (1996). 520 3# ‡aComplex analysis of geomorphological glacial processes in forefields of retreating glaciers was undertaken. Field studies and archival cartographic materials indicate continued glacial retreat, at least since turn of century. Average rate is now 20 m/yr, with no moraine ridges formed, except for fluted moraines. At present glaciofluvial erosion predominates. 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc 650 07 ‡a551.331 -- Glacial erosion.‡2udc 650 07 ‡a551.332.58 -- Outwash plains.‡2udc 650 07 ‡a556.51 -- River basins and watersheds.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*32) -- Svalbard.‡2udc 773 0# ‡7nnas ‡tPolish Polar Research. ‡gVol. 17(1-2) (1996) ‡wSPRI-60789 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231003