Estuarine–fluvial floodplain formation in the Holocene Lower Tagus valley (Central Portugal) and implications for Quaternary fluvial system evolution

2007 ◽  
Vol 26 (22-24) ◽  
pp. 2937-2957 ◽  
Author(s):  
Tim van der Schriek ◽  
David G. Passmore ◽  
Jose Rolão ◽  
Anthony C. Stevenson
Keyword(s):  
Fluvial System ◽  
The Holocene ◽  
System Evolution ◽  
Lower Tagus Valley ◽  
Central Portugal ◽  
Tagus Valley

Fluvial system evolution and environmental changes during the Holocene in the Mue valley (Western France)

Geomorphology ◽  
2008 ◽  
Vol 98 (1-2) ◽  
pp. 55-70 ◽  
Author(s):  
Laurent Lespez ◽  
Martine Clet-Pellerin ◽  
Nicole Limondin-Lozouet ◽  
Jean-François Pastre ◽  
Michel Fontugne ◽  
...  
Keyword(s):  
Environmental Changes ◽  
Fluvial System ◽  
The Holocene ◽  
System Evolution

scholarly journals The Eastern Lower Tagus Valley Fault Zone in central Portugal: Active faulting in a low-deformation region within a major river environment

2015 ◽  
Vol 660 ◽  
pp. 117-131 ◽  
Author(s):  
Carolina Canora ◽  
Susana P. Vilanova ◽  
Glenda M. Besana-Ostman ◽  
João Carvalho ◽  
Sandra Heleno ◽  
...  
Keyword(s):  
Fault Zone ◽  
Active Faulting ◽  
Deformation Region ◽  
Lower Tagus Valley ◽  
Central Portugal ◽  
Major River ◽  
Tagus Valley

Large Holocene Earthquakes in the Lower Tagus Valley Fault Zone, Central Portugal

2012 ◽  
Vol 83 (1) ◽  
pp. 67-76 ◽  
Author(s):  
G. M. Besana-Ostman ◽  
S. P. Vilanova ◽  
E. S. Nemser ◽  
A. Falcao-Flor ◽  
S. Heleno ◽  
...  
Keyword(s):  
Fault Zone ◽  
Lower Tagus Valley ◽  
Central Portugal ◽  
Tagus Valley

scholarly journals The Azambuja fault: An active structure located in an intraplate basin with significant seismicity (Lower Tagus Valley, Portugal)

2004 ◽  
Vol 8 (3) ◽  
pp. 347-362 ◽  
Author(s):  
J. Cabral ◽  
P. Ribeiro ◽  
P. Figueiredo ◽  
N. Pimentel ◽  
A. Martins
Keyword(s):  
Active Structure ◽  
Lower Tagus Valley ◽  
Tagus Valley

scholarly journals Specific Exogenetic (External) and Endogenetic (Internal) Effects on Fluvial System Evolution

Quaternary ◽  
2018 ◽  
Vol 1 (3) ◽  
pp. 27 ◽  
Author(s):  
Jef Vandenberghe ◽  
David Bridgland ◽  
Xianyan Wang
Keyword(s):  
Direct Effects ◽  
Fluvial System ◽  
Special Issue ◽  
High Complexity ◽  
External Effects ◽  
System Evolution ◽  
Fluvial Dynamics ◽  
External Variables ◽  
Fluvial Archives ◽  
Made In

A collection of papers appears under the title “Special External Effects on Fluvial System Evolution” in the journal, Quaternary. This is a new Special Issue under the aegis of the Fluvial Archives Group (FLAG), illustrating the recent progress made in paleo-fluvial research. These papers highlight the high complexity of the external forcing of fluvial dynamics, and especially, the combined results of several interfering variables. In addition, it appears that the study of fluvial archives cannot be limited to the general and direct effects of external variables, but it also has to include the indirect influences that are regionally variable.

Seismic hazard impact of the Lower Tagus Valley Fault Zone (SW Iberia)

2004 ◽  
Vol 8 (3) ◽  
pp. 331-345 ◽  
Author(s):  
Susana P. Vilanova ◽  
Joao F.B.D. Fonseca
Keyword(s):  
Seismic Hazard ◽  
Fault Zone ◽  
Lower Tagus Valley ◽  
Tagus Valley

Evidence of Stream Response to Holocene Climatic Change in a Small Wisconsin Watershed

1983 ◽  
Vol 19 (1) ◽  
pp. 100-116 ◽  
Author(s):  
Patricia F. McDowell
Keyword(s):  
Simple Model ◽  
Climatic Change ◽  
Climatic Changes ◽  
Soil Development ◽  
Fluvial System ◽  
Alluvial Deposits ◽  
The Holocene ◽  
Fluvial Response ◽  
Stream Response ◽  
The Relationship

AbstractDuring the Holocene, moderate climatic and vegetational changes triggered several episodes of adjustment in the Brush Creek fluvial system. The alluvial chronology includes an episode of erosion at 7800 – 5700 yr B.P. corresponding to the mid-Holocene precipitation minimum and an episode of floodplain construction at 5700 – 5000 yr B.P. corresponding to a rapid increase in precipitation. Holocene climatic changes have influenced the sedimentology of the alluvial deposits and soil development on them. Fluvial adjustment is caused primarily by hydrologic and hydraulic changes related to climatic change, but there is no simple model for fluvial response to climatic change. The relationship between the direction of climatic change and the type of fluvial response is complex.

scholarly journals Ground-Motion Simulation in the Lower Tagus Valley Basin

2015 ◽  
Vol 172 (9) ◽  
pp. 2411-2420 ◽  
Author(s):  
J. F. Borges ◽  
M. Bezzeghoud ◽  
B. Caldeira ◽  
João Carvalho
Keyword(s):  
Ground Motion ◽  
Motion Simulation ◽  
Ground Motion Simulation ◽  
Lower Tagus Valley ◽  
Tagus Valley
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