Late Holocene great earthquakes and relative sea-level change at Kenai, southern Alaska

2005 ◽  
Vol 20 (2) ◽  
pp. 95-111 ◽  
Author(s):  
Sarah Hamilton ◽  
Ian Shennan
Keyword(s):  
Sea Level ◽  
Late Holocene ◽  
Sea Level Change ◽  
Relative Sea Level ◽  
Level Change ◽  
Great Earthquakes

scholarly journals Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Anders Schomacker ◽  
Wesley R. Farnsworth ◽  
Ólafur Ingólfsson ◽  
Lis Allaart ◽  
Lena Håkansson ◽  
...  
Keyword(s):  
Sea Level ◽  
Late Holocene ◽  
Sea Level Change ◽  
Relative Sea Level ◽  
Level Change

scholarly journals POSTGLACIAL RELATIVE SEA LEVEL CHANGE AND GLACIER ACTIVITY IN THE EARLY AND LATE HOLOCENE: WAHLENBERGFJORDEN, NORDAUSTLANDET, SVALBARD

2019 ◽  
Author(s):  
Anders Schomacker ◽  
◽  
Wesley R. Farnsworth ◽  
Ólafur Ingólfsson ◽  
Lis Allaart ◽  
...  
Keyword(s):  
Sea Level ◽  
Late Holocene ◽  
Sea Level Change ◽  
Relative Sea Level ◽  
Level Change

scholarly journals Late Glacial to Holocene relative sea-level change in Assynt, northwest Scotland, UK

2015 ◽  
Vol 84 (2) ◽  
pp. 214-222 ◽  
Author(s):  
Christine A. Hamilton ◽  
Jeremy M. Lloyd ◽  
Natasha L.M. Barlow ◽  
James B. Innes ◽  
Rachel Flecker ◽  
...  
Keyword(s):  
Sea Level ◽  
Late Holocene ◽  
Sea Level Change ◽  
Late Glacial ◽  
Test Model ◽  
Relative Sea Level ◽  
Level Change ◽  
Isostatic Adjustment ◽  
Global And Local ◽  
First Time

Relative sea-level change (RSL), from the Late Glacial through to the late Holocene, is reconstructed for the Assynt region, northwest Scotland, based on bio- and lithostratigraphical analysis. Four new radiocarbon-dated sea-level index points help constrain RSL change for the Late Glacial to the late Holocene. These new data, in addition to published material, capture the RSL fall during the Late Glacial and the rise and fall associated with the mid-Holocene highstand. Two of these index points constrain the Late Glacial RSL history in Assynt for the first time, reconstructing RSL falling from 2.47 ± 0.59 m OD to 0.15 ± 0.59 m OD at c. 14,000–15,000 cal yr BP. These new data test model predictions of glacial isostatic adjustment (GIA), particularly during the early deglacial period which is currently poorly constrained throughout the British Isles. Whilst the empirical data from the mid- to late-Holocene to present matches quite well with the recent GIA model output, there is a relatively poor fit between the timing of the Late Glacial RSL fall and early Holocene RSL rise. This mismatch, also evident elsewhere in northwest Scotland, may result from uncertainties associated with both the global and local ice components of GIA models.

Sedimentary record of late-Holocene relative sea-level change and tectonic deformation from the Guerrero Seismic Gap, Mexican Pacific Coast

The Holocene ◽  
2007 ◽  
Vol 17 (8) ◽  
pp. 1211-1220 ◽  
Author(s):  
M. Teresa Ramirez-Herrera ◽  
Andrew Cundy ◽  
Vladimir Kostoglodov ◽  
Arturo Carranza-Edwards ◽  
Eduardo Morales ◽  
...  
Keyword(s):  
Sea Level ◽  
Late Holocene ◽  
Pacific Coast ◽  
Sea Level Change ◽  
Tectonic Deformation ◽  
Seismic Gap ◽  
Sedimentary Record ◽  
Relative Sea Level ◽  
Mexican Pacific ◽  
Level Change

Late Quaternary sea levels and crustal movements, coastal British Columbia

1982 ◽  
Vol 19 (3) ◽  
pp. 597-618 ◽  
Author(s):  
John Clague ◽  
John R. Harper ◽  
R. J. Hebda ◽  
D. E. Howes
Keyword(s):  
British Columbia ◽  
Sea Level ◽  
Late Holocene ◽  
Late Quaternary ◽  
Sea Level Change ◽  
Vancouver Island ◽  
Relative Sea Level ◽  
Crustal Movements ◽  
Level Change ◽  
Queen Charlotte Islands

Late Quaternary sea-level fluctuations on the British Columbia coast have been established from studies of terrestrial and marine sediments and landforms. These studies indicate that the sea-level history of mainland British Columbia and eastern Vancouver Island is very different from that of the Queen Charlotte Islands and western Vancouver Island. Specifically, in the former areas, there was a rapid rise of submerged coastal lowlands between about 13 000 and 10 000 years ago. Emergence culminated about 6000–9000 years ago, depending on the locality, when the sea, relative to the land, was 12 m or more lower than at present in some areas. During middle and late Holocene time, relative sea level rose on the mainland coast and at least locally on eastern Vancouver Island, resulting in inundation of coastal archaeological sites and low-lying terrestrial vegetation. Tidal records and precise levelling suggest ongoing submergence of at least part of this region.In contrast, shorelines on the Queen Charlotte Islands were below present from before 13 700 years ago until approximately 9500–10 000 years ago. A transgression at the close of the Pleistocene climaxed about 7500–8500 years ago when relative sea level probably was about 15 m above present in most areas. Most of the emergence that followed apparently occurred in the last 5000–6000 years. There has been a similar pattern of emergence on the west coast of Vancouver Island during late Holocene time.The above patterns of late Quaternary sea-level change are attributed to complex isostatic response to downwasting and retreat of the late Wisconsin Cordilleran Ice Sheet, to transfers of water from melting ice sheets to oceans, and to plate interactions on the British Columbia continental margin. Late Pleistocene and early Holocene crustal movements were dominantly isostatic. Although the recent regression on the outer coast likely is due, at least in part, to tectonic uplift, some late Holocene sea-level change in this area and elsewhere on the British Columbia coast may be either eustatic in nature or a residual isostatic response to deglaciation, which occurred thousands of years earlier.

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