Zobrazeno 1 - 10 of 30 pro vyhledávání: '"D. G. Sutherland"'
1
Scotland
Autor: D. G. Sutherland
Publikováno v: A revised correlation of Quaternary deposits in the British Isles ISBN: 9781862390423
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d0d2feeb7963c88b8ab1653b31fc4f2b
https://doi.org/10.1144/sr23.9
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2
Forest burial by large rock avalanche in Miller Stream, Seaward Kaikoura Range, New Zealand, c. 1700 years ago
Autor: J. L. Redwine, Russell J. vanDissen, D. G. Sutherland, R. J. Bowers
Publikováno v: Scopus-Elsevier
A forest buried at 1630–1730 cal. BP has been exhumed by incision of Miller Stream, a tributary of Clarence River that drains the steep southeast flank of the Seaward Kaikoura Range, Marlborough, New Zealand. The paleofor‐est is exposed along sev
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b05b04fa0c99620e847a4d5008c0caa5
https://doi.org/10.1080/00288306.2006.9515155
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4
North-east Scotland
Autor: D. E. Smith, J. E. Gordon, J. Jarvis, D. G. Sutherland, A. M. Hall
Publikováno v: Quaternary of Scotland ISBN: 9789401046572
North-east Scotland covers the mainly lowland area between lower Strathspey and Aberdeen (Figure 8.1). Geologically, it is underlain by the same Dalradian metamorphic rocks and younger granitic intrusions as the central and south-west Highlands, and
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9890b7057651c925a08e7db7642010fe
https://doi.org/10.1007/978-94-011-1500-1_8
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5
Lothians and Borders
Autor: P. D. Moore, D. G. Sutherland, John E. Gordon, Harry John Betteley Birks
Publikováno v: Quaternary of Scotland ISBN: 9789401046572
This area includes the lowlands of the Lothians along the southern shore of the Firth of Forth and the coastal area south to Berwick (Figure 17.1). Inland it extends west to the A74 across the Southern Uplands and south to the Tweed Valley. The area
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::e98a715764c32706db490986e680df90
https://doi.org/10.1007/978-94-011-1500-1_17
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6
Eastern Highland Boundary
Autor: C. J. Caseldine, L. J. McEwen, D. G. Sutherland, D. E. Smith, John E. Gordon
Publikováno v: Quaternary of Scotland ISBN: 9789401046572
The Eastern Highland Boundary region extends from west of Perth and the Tay Valley through Strathmore to Aberdeen (Figure 14.1). It incorporates the coastline from south of Montrose to Aberdeen. Glaciation of the area has been dominantly by ice origi
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5ebfc3fbd015dd48d052833e96ea6cfb
https://doi.org/10.1007/978-94-011-1500-1_14
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7
South-west Scotland
Autor: V. J. Jones, A. C. Stevenson, John E. Gordon, D. G. Sutherland, Hjb Birks
Publikováno v: Quaternary of Scotland ISBN: 9789401046572
Southwest Scotland comprises that part of the Southern Uplands west of the A74 and the coastal lowlands along the Solway Firth (Figure 18.1). Little is known of the Quaternary history of the area prior to the last, Devensian ice-sheet glaciation, alt
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::34a853c7eecbaa8b22d3892da374c93b
https://doi.org/10.1007/978-94-011-1500-1_18
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8
Fife and lower Tay
Autor: G. Whittington, P. R. Cundill, D. G. Sutherland, John E. Gordon, D. E. Smith, R. A. Cullingford, K. J. Edwards
Publikováno v: Quaternary of Scotland ISBN: 9789401046572
This area includes the peninsula of Fife between the Firth of Tay and Firth of Forth, the lower Tay valley and Strathearn (Figure 15.1). The low-lying coastal areas and the lower parts of the valleys contain extensive accumulations of Late-glacial an
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::45d856d93d549c3352a70dbe90a2b361
https://doi.org/10.1007/978-94-011-1500-1_15
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9
The Quaternary in Scotland
Autor: D. G. Sutherland, John E. Gordon
Publikováno v: Quaternary of Scotland ISBN: 9789401046572
The broad outlines of the Scottish landscape owe their origins to a combination of geological and tectonic controls and geomorphological processes in pre-Quaternary time. However, there are few on-land deposits that predate the Quaternary and the gre
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6edeeec838fb39429d9dfe8f30e161ef
https://doi.org/10.1007/978-94-011-1500-1_2
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