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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #126938:
- #126938
Main publication details
MARC recordPeriglacial environmental developments between 30 and 20 ka BP in Denmark / Else Kolstrup.
| Title: | Periglacial environmental developments between 30 and 20 ka BP in Denmark / Else Kolstrup. |
| Author(s): | Kolstrup, Else. |
| Date: | 1993. |
| Abstract: | Describes sedimentary sequence covering this time span. Composed of loess and sand-loess, alternating with waterlain sediments in lower part and with slope deposits in upper part. Evidence shows that there was much reworking of sediments by wind. Presence of slope deposits and frost-wedge casts points to permafrost (intermittent?) between 24 and 20 ka BP and possible between 27 and 24 ka BP. Vegetation was probably present throughout entire period. |
| Notes: | Offprint: Geologie en Mijnbouw. Vol. 72(2) :159-166. |
| Keywords: | 551.34 -- Geocryology. Frozen ground. 551.343 -- Periglacial processes. Thermokarst. 551.345.3 -- Permafrost, composition and structure. Ice wedges. 551.583.3 -- Climatic changes, Quaternary. E8 -- Glaciology: frost action and permafrost. (489) -- Denmark. |
| Location(s): | SCO: SPRI-SHF: 551.34 |
| SPRI record no.: | 126938 |
LDR 01371nam#a2200000#a#4500 001 SPRI-126938 005 20230924234940.0 007 ta 008 230924s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-126938 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aKolstrup, Else. 245 10 ‡aPeriglacial environmental developments between 30 and 20 ka BP in Denmark /‡cElse Kolstrup. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 159-166 :‡bdiags., map. 500 ## ‡aOffprint: Geologie en Mijnbouw. Vol. 72(2) :159-166. 520 3# ‡aDescribes sedimentary sequence covering this time span. Composed of loess and sand-loess, alternating with waterlain sediments in lower part and with slope deposits in upper part. Evidence shows that there was much reworking of sediments by wind. Presence of slope deposits and frost-wedge casts points to permafrost (intermittent?) between 24 and 20 ka BP and possible between 27 and 24 ka BP. Vegetation was probably present throughout entire period. 650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc 650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc 650 07 ‡a551.345.3 -- Permafrost, composition and structure. Ice wedges.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 651 #7 ‡a(489) -- Denmark.‡2udc 852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h551.34‡9Create 1 item record‡0Migrate 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230924