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Record #96774:
- #96774
Main publication details
MARC recordLate Devensian raised shorelines and ice limits in the inner Moray Firth area, northern Scotland / Callum R. Firth.
| Title: | Late Devensian raised shorelines and ice limits in the inner Moray Firth area, northern Scotland / Callum R. Firth. |
| Author(s): | Firth, Callum R. |
| Date: | 1989. |
| In: | Boreas. (1989.), Vol. 18(1) (1989) |
| Abstract: | Marine, fluvial and fluvioglacial landforms and deposits have been mapped in this area. Landforms indicate close association between decay of Late Devensian Scottish ice sheet and formation of raised marine features. Analysis of altitudes of marine terraces has identified ten glacio-isostatically tilted raised shorelines of Late Devensian age, sloping down N25°E, at progressively lower gradients between 0.57 and 0.15 m km⁻¹. Shorelines were formed in close association with westward- and southward-receding ice margin and shoreline sequence suggests that rates of ice-margin retreat were most rapid where ice terminated in sea. |
| Notes: | Boreas. Vol. 18(1) :5-21 (1989). |
| Keywords: | 551.336 -- Ice ages. 551.79 -- Quaternary. 551.35.054.13 -- Raised beaches. E7 -- Glaciology: glacial geology and ice ages. (411) -- Scotland. |
| SPRI record no.: | 96774 |
LDR 01418naa#a2200000#a#4500 001 SPRI-96774 005 20240419011543.0 007 ta 008 240419s1989####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-96774 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aFirth, Callum R. 245 10 ‡aLate Devensian raised shorelines and ice limits in the inner Moray Firth area, northern Scotland /‡cCallum R. Firth. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1989. 300 ## ‡ap. 5-21 :‡bdiags., tables, maps. 500 ## ‡aBoreas. Vol. 18(1) :5-21 (1989). 520 3# ‡aMarine, fluvial and fluvioglacial landforms and deposits have been mapped in this area. Landforms indicate close association between decay of Late Devensian Scottish ice sheet and formation of raised marine features. Analysis of altitudes of marine terraces has identified ten glacio-isostatically tilted raised shorelines of Late Devensian age, sloping down N25°E, at progressively lower gradients between 0.57 and 0.15 m km⁻¹. Shorelines were formed in close association with westward- and southward-receding ice margin and shoreline sequence suggests that rates of ice-margin retreat were most rapid where ice terminated in sea. 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.35.054.13 -- Raised beaches.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(411) -- Scotland.‡2udc 773 0# ‡7nnas ‡tBoreas. ‡gVol. 18(1) (1989) ‡wSPRI-56035 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419