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Record #112520:
- #112520
Main publication details
MARC recordThe extension of the Late Weichselian/Late Devensian ice sheets in the North Sea basin / Jürgen Ehlers, Robin Wingfield.
| Title: | The extension of the Late Weichselian/Late Devensian ice sheets in the North Sea basin / Jürgen Ehlers, Robin Wingfield. |
| Author(s): | Ehlers, Jürgen. Wingfield, Robin. |
| Date: | 1991. |
| In: | Journal of Quaternary Science : JQS. (1991.), Vol. 6(4) (1991) |
| Abstract: | Distribution of large channel-like features, comprising Weichselian/Devensian incisions, provide evidence for much larger extension of last ice sheet than assumed. Morphological comparison of incisions with those in north Germany and Poland reveal similarity in shape and distribution. Probably formed by meltwater erosion within margin of ice sheet. Absence of till may be due to later erosion. Large-scale reworking and redistribution of sediments is indicated by complete sediment infill of incisions. |
| Notes: | Journal of Quaternary Science : JQS. Vol. 6(4) :313-326 (1991). |
| Keywords: | 551.33 -- Glacial geology. 551.331.5 -- Glacial erosion and protection. Sub-glacial topography. 551.336 -- Ice ages. 551.79 -- Quaternary. .000(410) -- British author. E7 -- Glaciology: glacial geology and ice ages. (261.2) -- North Sea. |
| SPRI record no.: | 112520 |
LDR 01501naa#a2200000#a#4500 001 SPRI-112520 005 20230331133051.0 007 ta 008 230331s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-112520 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aEhlers, Jürgen. 245 14 ‡aThe extension of the Late Weichselian/Late Devensian ice sheets in the North Sea basin /‡cJürgen Ehlers, Robin Wingfield. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 313-326 :‡bdiags., maps. 500 ## ‡aJournal of Quaternary Science : JQS. Vol. 6(4) :313-326 (1991). 520 3# ‡aDistribution of large channel-like features, comprising Weichselian/Devensian incisions, provide evidence for much larger extension of last ice sheet than assumed. Morphological comparison of incisions with those in north Germany and Poland reveal similarity in shape and distribution. Probably formed by meltwater erosion within margin of ice sheet. Absence of till may be due to later erosion. Large-scale reworking and redistribution of sediments is indicated by complete sediment infill of incisions. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.331.5 -- Glacial erosion and protection. Sub-glacial topography.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a.000(410) -- British author.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(261.2) -- North Sea.‡2udc 700 1# ‡aWingfield, Robin. 773 0# ‡7nnas ‡tJournal of Quaternary Science : JQS. ‡gVol. 6(4) (1991) ‡wSPRI-78713 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230331