Zobrazeno 1 - 10
of 141
pro vyhledávání: '"R.W.G. Carter"'
Publikováno v:
Journal of Quaternary Science. 4:7-24
The course of Irish sea levels during the late-Holocene is not well-known, yet it is an understanding of this period that will prove crucial in the definition and management of future sea-level changes. The coastline of Ireland embraces wide environm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa535090d3d4ed1fec2107da36d116b6
https://doi.org/10.1002/jqs.3390040103
https://doi.org/10.1002/jqs.3390040103
Autor:
R.W.G. Carter
Publikováno v:
Boreas. 12:167-182
Products of marine processes occupy a considerable vertical range, which varies along the shore. Extreme waves can both cause erosion and form depositional structures up to several metres above the high tide mark. Temporary supra-elevation of water l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c0868c4fad92eefa2cfdad41c666da31
https://doi.org/10.1111/j.1502-3885.1983.tb00310.x
https://doi.org/10.1111/j.1502-3885.1983.tb00310.x
Autor:
John Shaw, R.W.G. Carter
Publikováno v:
Boreas. 23:74-91
Peat and organic rich sediments at coastal sites in extreme northwest Ireland have accumulated in a wide variety of environments, often strongly influenced by late Holocene changes in relative sea level and by geomorphic processes. A deep peat sequen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a0bab6ca9617638a0817c3f1782da4d
https://doi.org/10.1111/j.1502-3885.1994.tb00588.x
https://doi.org/10.1111/j.1502-3885.1994.tb00588.x
Publikováno v:
Sea Level Changes: Determination and Effects
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35a08b1bbda8fef9b034ec999cec472b
https://doi.org/10.1029/gm069p0071
https://doi.org/10.1029/gm069p0071
Publikováno v:
Marine Geology. 126:63-85
Beaches and barriers on many mid- to high-latitude coasts comprise mixtures of fine and coarse clastic materials forming a distinctive morphodynamic environment. In many cases, the sediments are derived primarily from limited glacigenic deposits and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f9f6c18dafb1bbeecc1980322ac23db9
https://doi.org/10.1016/0025-3227(95)00066-8
https://doi.org/10.1016/0025-3227(95)00066-8
Autor:
Julian D. Orford, R.W.G. Carter
Publikováno v:
Marine Geology. 126:201-211
The possibility by which the retreat of a swash-aligned, gravel barrier on Nova Scotia's Atlantic coast may be influenced by varying mesoscale time domains of differential process conditions is examined. Tide gauge data are used to generate definitio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a47bca6fc9c7a3e7663f7220436bc944
https://doi.org/10.1016/0025-3227(95)00078-d
https://doi.org/10.1016/0025-3227(95)00078-d
Publikováno v:
Marine Geology. 124:129-136
Paraglacial coastlines with dynamic, coarse clastic barrier beaches are common in mid- to high-latitudes today, and have been during the Holocene. Sediments that have been deposited along these coastlines, often in back-barrier locations, have been u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a88b15dc9c2673d71e91e9d10d83fee
https://doi.org/10.1016/0025-3227(95)00036-x
https://doi.org/10.1016/0025-3227(95)00036-x
Publikováno v:
Marine Geology. 124:177-186
In theory, a rise in sea level should force swash-aligned gravel-barriers to retreat landwards. Evidence from three single-crested, swash-aligned gravel barriers from eastern Canada and northwest Europe indicates that barrier-retreat rate correlates
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::620ffe8b61bb617a0cca948436382739
https://doi.org/10.1016/0025-3227(95)00039-2
https://doi.org/10.1016/0025-3227(95)00039-2
Publikováno v:
Earth Surface Processes and Landforms. 20:21-37
Sea-level rise (SLR) is considered to be important for barrier behaviour when barriers are swash-aligned and single-crested, which is typical of only one part of a barrier's lifeterm. Under such conditions gravel-barrier retreat rate correlates with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2bd64b41ca8cc6a948403dd88bf01aa2
https://doi.org/10.1002/esp.3290200104
https://doi.org/10.1002/esp.3290200104
Publikováno v:
Marine Geology. 117:19-34
At Portballintrae, Northern Ireland, a well-preserved emergent facies sequence formed around 17 kyr B.P. as the Late Devensian ice sheet withdrew from the continental shelf. Three main lithofacies assemblages are recognised: (1) At the base of the se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a9fc305046001739b229a8a64e86e63d
https://doi.org/10.1016/0025-3227(94)90004-3
https://doi.org/10.1016/0025-3227(94)90004-3