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Record #146569:
- #146569
Main publication details
MARC recordThe glacial geomorphology of central and northern Sweden / Clas Hättestrand.
| Title: | The glacial geomorphology of central and northern Sweden / Clas Hättestrand. |
| Author(s): | Hättestrand, Clas. |
| Date: | 1998. |
| In: | SGU. Research Papers. Series Ca. (1998.), Ca 85 (1998) |
| Abstract: | Glacial geomorphology of area mostly records decay of Fennoscandian ice sheet during Late Weichselian deglaciation. As ice margin retreated, glacial landforms were formed. De Geer moraines also occur in many parts of area below highest post-glacial shoreline. Within cold based zones, meltwater channels are superimposed on older landscapes. In eastern part of Scandinavian mountains, segments of large lateral moraines are found, marking upper surface of outlet glaciers draining eastwards. In central and western parts of chain, much of ice sheet seems to have been fully warm-based and scouring its bed. |
| Notes: | SGU. Research Papers. Series Ca. Ca 85 :1-47 (1998). |
| Keywords: | 551.332.5 -- Glacial landforms. 551.4 -- Geomorphology. B -- Geology and soil sciences. (*3) -- Arctic regions. (*57) -- Sweden. |
| SPRI record no.: | 146569 |
LDR 01388naa#a2200000#a#4500 001 SPRI-146569 005 20240416164602.0 007 ta 008 240416s1998####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-146569 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHättestrand, Clas. 245 14 ‡aThe glacial geomorphology of central and northern Sweden /‡cClas Hättestrand. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1998. 300 ## ‡ap. 1-47 :‡bill., maps (one in pocket) 500 ## ‡aSGU. Research Papers. Series Ca. Ca 85 :1-47 (1998). 520 3# ‡aGlacial geomorphology of area mostly records decay of Fennoscandian ice sheet during Late Weichselian deglaciation. As ice margin retreated, glacial landforms were formed. De Geer moraines also occur in many parts of area below highest post-glacial shoreline. Within cold based zones, meltwater channels are superimposed on older landscapes. In eastern part of Scandinavian mountains, segments of large lateral moraines are found, marking upper surface of outlet glaciers draining eastwards. In central and western parts of chain, much of ice sheet seems to have been fully warm-based and scouring its bed. 650 07 ‡a551.332.5 -- Glacial landforms.‡2udc 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*57) -- Sweden.‡2udc 773 0# ‡7nnas ‡tSGU. Research Papers. Series Ca. ‡gCa 85 (1998) ‡wSPRI-9682 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416