Slope-Channel Coupling as a Factor in the Evolution of Mountains The Western Carpathians and Sudetes /

In this thesis, coupling between the delivery of slope material into valley floors and river erosion is considered to be a factor in the evolution of mid-altitude, forested mountains. Analyses of slope-channel interactions were made in ten small catchments with particular emphasis on landsliding-ero...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Wistuba, Małgorzata (Autor)
Autor Corporativo: SpringerLink (Online service)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Cham : Springer International Publishing : Imprint: Springer, 2014.
Edición:1st ed. 2014.
Colección:Springer Theses, Recognizing Outstanding Ph.D. Research,
Temas:
Geomorphology.
Physical geography.
Earth System Sciences.
Acceso en línea:Texto Completo

MARC

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100 1 |a Wistuba, Małgorzata.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
245 1 0 |a Slope-Channel Coupling as a Factor in the Evolution of Mountains  |h [electronic resource] :  |b The Western Carpathians and Sudetes /  |c by Małgorzata Wistuba. 
250 |a 1st ed. 2014. 
264 1 |a Cham :  |b Springer International Publishing :  |b Imprint: Springer,  |c 2014. 
300 |a XIII, 224 p. 109 illus., 39 illus. in color.  |b online resource. 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
347 |a text file  |b PDF  |2 rda 
490 1 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5061 
505 0 |a Introduction -- Materials and methods -- Study catchments -- The delivery of slope material to the valley floors of small mid-mountain catchments - record in relief and deposits -- The evolution of relief in mid-altitude mountains as a result of the delivery of slope material to valley floors - discussion -- Conclusions. 
520 |a In this thesis, coupling between the delivery of slope material into valley floors and river erosion is considered to be a factor in the evolution of mid-altitude, forested mountains. Analyses of slope-channel interactions were made in ten small catchments with particular emphasis on landsliding-erosion feedback. An original, new dendrogeomorphic approach was applied to determine the cyclic occurrence of landsliding and erosion during recent decades. The results of dendrochronological studies show that the processes studied are strongly interdependent. Fluvial erosion can trigger landsliding by undermining slope bases. Landsliding can intensify erosion by delivering slope material into valley floors. The results of dendrochronological studies have permitted a better understanding of the relief observed in areas where landslides and erosion are coupled. A scheme was established  which describes the importance of coupling in the evolution of mid-mountain landscape. 
650 0 |a Geomorphology. 
650 0 |a Physical geography. 
650 1 4 |a Geomorphology. 
650 2 4 |a Earth System Sciences. 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer Nature eBook 
776 0 8 |i Printed edition:  |z 9783319058207 
776 0 8 |i Printed edition:  |z 9783319058184 
776 0 8 |i Printed edition:  |z 9783319382968 
830 0 |a Springer Theses, Recognizing Outstanding Ph.D. Research,  |x 2190-5061 
856 4 0 |u https://doi.uam.elogim.com/10.1007/978-3-319-05819-1  |z Texto Completo 
912 |a ZDB-2-EES 
912 |a ZDB-2-SXEE 
950 |a Earth and Environmental Science (SpringerNature-11646) 
950 |a Earth and Environmental Science (R0) (SpringerNature-43711) 

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