The Islands of Islay, Jura, Colonsay, Tiree and Coll
The Hebridean islands of Islay, Jura and Colonsay are mainly composed of Neoproterozoic metasedimentary rocks of the Dalradian supergroup, whereas Tiree and Coll are underlain by Archaean rocks of the Lewisian Gneiss Complex. Most of the terrain is low-lying; only the three peaks of the Paps of Jura...
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ftunivdundeepure:oai:discovery.dundee.ac.uk:publications/d33aaaa9-9524-4a76-a1b1-e0e4fb7668ef 2024-06-23T07:53:46+00:00 The Islands of Islay, Jura, Colonsay, Tiree and Coll Dawson, Alastair G. Ballantyne, Colin K. Ballantyne, Colin K. Gordon, John E. 2021 https://discovery.dundee.ac.uk/en/publications/d33aaaa9-9524-4a76-a1b1-e0e4fb7668ef https://doi.org/10.1007/978-3-030-71246-4_11 http://www.scopus.com/inward/record.url?scp=85114092441&partnerID=8YFLogxK eng eng Springer https://discovery.dundee.ac.uk/en/publications/d33aaaa9-9524-4a76-a1b1-e0e4fb7668ef urn:ISBN:9783030712457 (hbk) urn:ISBN:9783030712488 (pbk) info:eu-repo/semantics/restrictedAccess Dawson , A G & Ballantyne , C K 2021 , The Islands of Islay, Jura, Colonsay, Tiree and Coll . in C K Ballantyne & J E Gordon (eds) , Landscapes and Landforms of Scotland . 1 edn , World Geomorphological Landscapes , Springer , Switzerland , pp. 219-232 . https://doi.org/10.1007/978-3-030-71246-4_11 Glacimarine deposits Glacio-isostatic uplift Machair Medial moraine Paraglacial rock-slope failures Raised beaches Rock platforms Strandflat /dk/atira/pure/subjectarea/asjc/1900/1907 name=Geology /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes bookPart 2021 ftunivdundeepure https://doi.org/10.1007/978-3-030-71246-4_11 2024-06-11T15:00:32Z The Hebridean islands of Islay, Jura and Colonsay are mainly composed of Neoproterozoic metasedimentary rocks of the Dalradian supergroup, whereas Tiree and Coll are underlain by Archaean rocks of the Lewisian Gneiss Complex. Most of the terrain is low-lying; only the three peaks of the Paps of Jura exceed 600 m. Successive episodes of ice-sheet glaciation have produced areas of ice-moulded topography, and retreat of the last (Late Devensian) ice sheet was accompanied by the deposition of outwash deposits and moraines, including the longest medial moraine in Scotland. The most impressive and internationally renowned landforms on the islands are those related to coastal erosion and deposition: high-level glacimarine deposits; ancient (possibly Pliocene) glaciated strandflat; extensive areas of high rock platforms and intertidal platforms that demonstrably pre-date the last ice sheet; an isostatically tilted rock platform that formed under Lateglacial periglacial conditions; magnificent flights of Lateglacial shingle ridges extending up to 37 m above present sea level; and lower Holocene raised beaches locally backed by sand dunes and areas of machair (calcareous aeolian shell-sand) deposits. Inland, the quartzite flanks of the Paps of Jura are scarred by paraglacial landslides possibly triggered by seismic activity that accompanied rapid glacio-isostatic uplift. Book Part Ice Sheet Discovery - University of Dundee Online Publications High Rock ENVELOPE(-111.452,-111.452,58.917,58.917) Islay ENVELOPE(59.717,59.717,-67.350,-67.350) Jura ENVELOPE(13.501,13.501,68.062,68.062) 219 232 |
institution |
Open Polar |
collection |
Discovery - University of Dundee Online Publications |
op_collection_id |
ftunivdundeepure |
language |
English |
topic |
Glacimarine deposits Glacio-isostatic uplift Machair Medial moraine Paraglacial rock-slope failures Raised beaches Rock platforms Strandflat /dk/atira/pure/subjectarea/asjc/1900/1907 name=Geology /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes |
spellingShingle |
Glacimarine deposits Glacio-isostatic uplift Machair Medial moraine Paraglacial rock-slope failures Raised beaches Rock platforms Strandflat /dk/atira/pure/subjectarea/asjc/1900/1907 name=Geology /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes Dawson, Alastair G. Ballantyne, Colin K. The Islands of Islay, Jura, Colonsay, Tiree and Coll |
topic_facet |
Glacimarine deposits Glacio-isostatic uplift Machair Medial moraine Paraglacial rock-slope failures Raised beaches Rock platforms Strandflat /dk/atira/pure/subjectarea/asjc/1900/1907 name=Geology /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes |
description |
The Hebridean islands of Islay, Jura and Colonsay are mainly composed of Neoproterozoic metasedimentary rocks of the Dalradian supergroup, whereas Tiree and Coll are underlain by Archaean rocks of the Lewisian Gneiss Complex. Most of the terrain is low-lying; only the three peaks of the Paps of Jura exceed 600 m. Successive episodes of ice-sheet glaciation have produced areas of ice-moulded topography, and retreat of the last (Late Devensian) ice sheet was accompanied by the deposition of outwash deposits and moraines, including the longest medial moraine in Scotland. The most impressive and internationally renowned landforms on the islands are those related to coastal erosion and deposition: high-level glacimarine deposits; ancient (possibly Pliocene) glaciated strandflat; extensive areas of high rock platforms and intertidal platforms that demonstrably pre-date the last ice sheet; an isostatically tilted rock platform that formed under Lateglacial periglacial conditions; magnificent flights of Lateglacial shingle ridges extending up to 37 m above present sea level; and lower Holocene raised beaches locally backed by sand dunes and areas of machair (calcareous aeolian shell-sand) deposits. Inland, the quartzite flanks of the Paps of Jura are scarred by paraglacial landslides possibly triggered by seismic activity that accompanied rapid glacio-isostatic uplift. |
author2 |
Ballantyne, Colin K. Gordon, John E. |
format |
Book Part |
author |
Dawson, Alastair G. Ballantyne, Colin K. |
author_facet |
Dawson, Alastair G. Ballantyne, Colin K. |
author_sort |
Dawson, Alastair G. |
title |
The Islands of Islay, Jura, Colonsay, Tiree and Coll |
title_short |
The Islands of Islay, Jura, Colonsay, Tiree and Coll |
title_full |
The Islands of Islay, Jura, Colonsay, Tiree and Coll |
title_fullStr |
The Islands of Islay, Jura, Colonsay, Tiree and Coll |
title_full_unstemmed |
The Islands of Islay, Jura, Colonsay, Tiree and Coll |
title_sort |
islands of islay, jura, colonsay, tiree and coll |
publisher |
Springer |
publishDate |
2021 |
url |
https://discovery.dundee.ac.uk/en/publications/d33aaaa9-9524-4a76-a1b1-e0e4fb7668ef https://doi.org/10.1007/978-3-030-71246-4_11 http://www.scopus.com/inward/record.url?scp=85114092441&partnerID=8YFLogxK |
long_lat |
ENVELOPE(-111.452,-111.452,58.917,58.917) ENVELOPE(59.717,59.717,-67.350,-67.350) ENVELOPE(13.501,13.501,68.062,68.062) |
geographic |
High Rock Islay Jura |
geographic_facet |
High Rock Islay Jura |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Dawson , A G & Ballantyne , C K 2021 , The Islands of Islay, Jura, Colonsay, Tiree and Coll . in C K Ballantyne & J E Gordon (eds) , Landscapes and Landforms of Scotland . 1 edn , World Geomorphological Landscapes , Springer , Switzerland , pp. 219-232 . https://doi.org/10.1007/978-3-030-71246-4_11 |
op_relation |
https://discovery.dundee.ac.uk/en/publications/d33aaaa9-9524-4a76-a1b1-e0e4fb7668ef urn:ISBN:9783030712457 (hbk) urn:ISBN:9783030712488 (pbk) |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1007/978-3-030-71246-4_11 |
container_start_page |
219 |
op_container_end_page |
232 |
_version_ |
1802645586380324864 |