Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView 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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #130424:
- #130424
Main publication details
MARC recordBoulder depressions in central Sweden -- remnants of a pre-Late Weichselian landscape? / Clas Hättestrand.
| Title: | Boulder depressions in central Sweden -- remnants of a pre-Late Weichselian landscape? / Clas Hättestrand. |
| Author(s): | Hättestrand, Clas. |
| Date: | 1994. |
| In: | Geografiska Annaler. Series A. Physical Geography. (1994.), Vol. 76A(3) (1994) |
| Abstract: | These are boulder-filled shallow depressions created by frost heave in loose deposits. Shows that areas of directional moraine (signs of active warm-based ice) lack boulder depressions. Could be results of two possibilities: unfavourable conditions for boulder depression formation in drumlinized/Rogen moraine areas, or differential Late Weichselian erosion of pre-existing evenly distributed boulder depressions. Concludes that second alternative is most likely. |
| Notes: | Geografiska Annaler. Series A. Physical Geography. Vol. 76A(3) :153-160 (1994). |
| Keywords: | 551.33 -- Glacial geology. 551.331.5 -- Glacial erosion and protection. Sub-glacial topography. E7 -- Glaciology: glacial geology and ice ages. (*57) -- Sweden. |
| SPRI record no.: | 130424 |
LDR 01341naa#a2200000#a#4500 001 SPRI-130424 005 20240419054956.0 007 ta 008 240419s1994####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-130424 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHättestrand, Clas. 245 10 ‡aBoulder depressions in central Sweden -- remnants of a pre-Late Weichselian landscape? /‡cClas Hättestrand. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1994. 300 ## ‡ap. 153-160 :‡bill., diag., maps. 500 ## ‡aGeografiska Annaler. Series A. Physical Geography. Vol. 76A(3) :153-160 (1994). 520 3# ‡aThese are boulder-filled shallow depressions created by frost heave in loose deposits. Shows that areas of directional moraine (signs of active warm-based ice) lack boulder depressions. Could be results of two possibilities: unfavourable conditions for boulder depression formation in drumlinized/Rogen moraine areas, or differential Late Weichselian erosion of pre-existing evenly distributed boulder depressions. Concludes that second alternative is most likely. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.331.5 -- Glacial erosion and protection. Sub-glacial topography.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*57) -- Sweden.‡2udc 773 0# ‡7nnas ‡tGeografiska Annaler. Series A. Physical Geography. ‡gVol. 76A(3) (1994) ‡wSPRI-40621 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419