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Record #110193:
- #110193
Main publication details
MARC recordLate Devensian glacial deposits and glaciations in eastern England and the adjoining offshore region / John A. Catt.
| Title: | Late Devensian glacial deposits and glaciations in eastern England and the adjoining offshore region / John A. Catt. |
| Author(s): | Catt, John A. |
| Date: | 1991. |
| Publisher: | Rotterdam, Brookfield: A.A. Balkema |
| In: | Glacial deposits in Great Britain and Ireland. (1991.), |
| Abstract: | Tills, glaciofluvial and glaciolacustrine deposits cover much of area between Scottish border and north Norfolk coast, as well as large areas of adjacent North Sea floor, due to major glaciation that occurred during Late Devensian time known as Dimlington Stadial; this must be assumed to be only glaciation of eastern England during Dimlington. Discusses evidence for ice movements on land at this time and distribution of surface and offshore deposits. Text references to other publications at end of volume. |
| Notes: | In: Glacial deposits in Great Britain and Ireland / Jürgen Ehlers, Philip L. Gibbard, Jim Rose, eds. |
| Keywords: | 551.33 -- Glacial geology. 551.332.2 -- Drift, glacial. Deposits. 551.332.212 -- Till or boulder clay. 551.332.24 -- Glacio-fluvial deposits. 551.332.26 -- Glacio-lacustrine deposits and varves. 551.336 -- Ice ages. 551.79 -- Quaternary. E7 -- Glaciology: glacial geology and ice ages. (420) -- England. |
| SPRI record no.: | 110193 |
LDR 01711naa#a2200000#a#4500 001 SPRI-110193 005 20230331082708.0 007 ta 008 230331s1991####ne#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-110193 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aCatt, John A. 245 10 ‡aLate Devensian glacial deposits and glaciations in eastern England and the adjoining offshore region /‡cJohn A. Catt. 260 ## ‡aRotterdam, Brookfield :‡bA.A. Balkema,‡c1991. 300 ## ‡ap. 61-68 :‡bill., maps. 500 ## ‡aIn: Glacial deposits in Great Britain and Ireland / Jürgen Ehlers, Philip L. Gibbard, Jim Rose, eds. 520 3# ‡aTills, glaciofluvial and glaciolacustrine deposits cover much of area between Scottish border and north Norfolk coast, as well as large areas of adjacent North Sea floor, due to major glaciation that occurred during Late Devensian time known as Dimlington Stadial; this must be assumed to be only glaciation of eastern England during Dimlington. Discusses evidence for ice movements on land at this time and distribution of surface and offshore deposits. Text references to other publications at end of volume. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc 650 07 ‡a551.332.212 -- Till or boulder clay.‡2udc 650 07 ‡a551.332.24 -- Glacio-fluvial deposits.‡2udc 650 07 ‡a551.332.26 -- Glacio-lacustrine deposits and varves.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(420) -- England.‡2udc 773 0# ‡7nnam ‡aJürgen Ehlers, Philip L. Gibbard, Jim Rose, eds. ‡tGlacial deposits in Great Britain and Ireland. ‡dRotterdam, Brookfield : A.A. Balkema, 1991. ‡wSPRI-110185 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230331