scholarly journals Holocene fluvial landscape evolution driven by sea level and tectonic controls in the Gangkou River, Hengchun Peninsula

2021 ◽  
Vol 32 (3) ◽  
pp. 339-360
Author(s):  
Jia-Hong Chen ◽  
Shyh-Jeng Chyi ◽  
Jiun-Yee Yen ◽  
Lih-Der Ho ◽  
Christopher Lüthgens ◽  
...  
Keyword(s):  
Sea Level ◽  
Landscape Evolution ◽  
Fluvial Landscape

scholarly journals Applying Pattern Oriented Sampling in current fieldwork practice to enable more effective model evaluation in fluvial landscape evolution research

2018 ◽  
Vol 43 (14) ◽  
pp. 2964-2980 ◽  
Author(s):  
Rebecca M. Briant ◽  
Kim M. Cohen ◽  
Stephane Cordier ◽  
Alain J.A.G. Demoulin ◽  
Mark G. Macklin ◽  
...  
Keyword(s):  
Model Evaluation ◽  
Landscape Evolution ◽  
Effective Model ◽  
Fluvial Landscape

Holocene sea-level changes and landscape evolution on the northern Carmel coast (Israel)

2005 ◽  
pp. 79-86 ◽  
Author(s):  
Ehud Galili ◽  
Dov Zviely ◽  
Mina Weinstein-Evron
Keyword(s):  
Sea Level ◽  
Landscape Evolution ◽  
Sea Level Changes ◽  
Holocene Sea Level

A midge-salinity transfer function for inferring sea level change and landscape evolution in the Hudson Bay Lowlands, Manitoba, Canada

2013 ◽  
Vol 51 (3) ◽  
pp. 325-341 ◽  
Author(s):  
Trapper R. Dickson ◽  
Darren G. Bos ◽  
Marlow G. Pellatt ◽  
Ian R. Walker
Keyword(s):  
Transfer Function ◽  
Sea Level ◽  
Landscape Evolution ◽  
Sea Level Change ◽  
Hudson Bay ◽  
Hudson Bay Lowlands ◽  
Level Change

scholarly journals Holocene sea-level change and coastal landscape evolution in the southern Gulf of Carpentaria, Australia

The Holocene ◽  
2018 ◽  
Vol 28 (9) ◽  
pp. 1411-1430 ◽  
Author(s):  
Craig R Sloss ◽  
Luke Nothdurft ◽  
Quan Hua ◽  
Shoshannah G O’Connor ◽  
Patrick T Moss ◽  
...  
Keyword(s):  
Sea Level ◽  
Landscape Evolution ◽  
Sea Level Change ◽  
Lower Latitude ◽  
Holocene Climate ◽  
Coastal Landscape ◽  
Sea Levels ◽  
Level Change ◽  
Rising Sea Levels ◽  
Holocene Sea Level

A revised Holocene sea-level history for the southern Gulf of Carpentaria is presented based on new data from the South Wellesley Archipelago and age recalibration of previous research. Results confirm that rising sea levels during the most recent post-glacial marine transgression breached the Arafura Sill ca. 11,700 cal. yr BP. Sea levels continued to rise to ca. –30 m by 10,000 cal. yr BP, leading to full marine conditions. By 7700 cal. yr BP, sea-level reached present mean sea-level (PMSL) and continued to rise to an elevation of between 1.5 m and 2 m above PMSL. Sea level remained ca. + 1.5 between 7000 and 4000 cal. yr BP, followed by rapid regression to within ± 0.5 m of PMSL by ca. 3500 cal. yr BP. When placed into a wider regional context results from this study show that coastal landscape evolution in the tropical north of Australia was not only dependent on sea-level change but also show a direct correlation with Holocene climate variability. Specifically, the formation and preservation of beach-rock deposits, intertidal successions, beach and chenier ridge systems hold valuable sea-level and Holocene climate proxies that can contribute to the growing research into lower latitude Holocene sea-level and climate histories.

Isostatic uplift driven by karstification and sea-level oscillation: Modeling landscape evolution in north Florida

Geology ◽  
2010 ◽  
Vol 38 (6) ◽  
pp. 531-534 ◽  
Author(s):  
Peter N. Adams ◽  
Neil D. Opdyke ◽  
John M. Jaeger
Keyword(s):  
Sea Level ◽  
Landscape Evolution ◽  
Isostatic Uplift ◽  
Level Oscillation ◽  
And Sea Level

scholarly journals Geomorphological Processes and Environmental Interpretation at Espalmador islet (Western Mediterranean)

2019 ◽  
Vol 7 (5) ◽  
pp. 144
Author(s):  
Laura del Valle Villalonga ◽  
Alida Timar-Gabor ◽  
Joan J. Fornós
Keyword(s):  
Sea Level ◽  
Marine Sediment ◽  
Wind Direction ◽  
Landscape Evolution ◽  
Sedimentary Facies ◽  
Western Mediterranean ◽  
Environmental Interpretation ◽  
Aeolian Activity ◽  
History Of ◽  
Geomorphological Processes

This study presents a sedimentological and stratigraphical description of the Pleistocene deposits cropping out in Espalmador islet (Illes Pitiüses). Four major sedimentary facies including the succession of aeolian, marine, colluvial and edaphic environments are described. The sedimentological and stratigraphical analysis of these deposits allows the reconstruction of the coastal Pleistocene environmental and geomorphological history of the Espalmador islet. The coastal relief and the fluctuations of the sea level mainly control the Pleistocene coastal landscape evolution on Espalmador. Episodes of aeolian activity and dune formation related to a predominant northwestern wind direction can be linked to periods of low sea level where a high amount of marine sediment is exposed on the shelf platform.

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