Geomorphological Setting of the Cordillera Blanca

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F24%3A10486540" target="_blank" >RIV/00216208:11310/24:10486540 - isvavai.cz</a>

Výsledek na webu

<a href="https://doi.org/10.1007/978-3-031-58245-5_2" target="_blank" >https://doi.org/10.1007/978-3-031-58245-5_2</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/978-3-031-58245-5_2" target="_blank" >10.1007/978-3-031-58245-5_2</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Geomorphological Setting of the Cordillera Blanca

Popis výsledku v původním jazyce

Surface processes and landforms in the Cordillera Blanca has been studied by several research teams over the years, especially because of the various types of natural hazards and glaciers that are found in the region. Pronounced neotectonic activity has influenced several geomorphological processes, such as fluvial erosion and slope movements. The landscape is usually highly dissected by processes influenced by endogenous activity (e.g., tectonic activity) as well as by exogenous processes (e.g., erosion and slope movements) whose intensity varies in space and time. Also, the large relief differences support the intensity of ongoing processes. Most dynamic processes are usually triggered by earthquakes or intensive precipitations (during the rainy season or El Niño period) and different processes can influence each other in terms of triggers. It is reasonable to expect that ongoing climate changes as well as deglaciation will influence future dynamic morphological processes.

Název v anglickém jazyce

Geomorphological Setting of the Cordillera Blanca

Popis výsledku anglicky

Surface processes and landforms in the Cordillera Blanca has been studied by several research teams over the years, especially because of the various types of natural hazards and glaciers that are found in the region. Pronounced neotectonic activity has influenced several geomorphological processes, such as fluvial erosion and slope movements. The landscape is usually highly dissected by processes influenced by endogenous activity (e.g., tectonic activity) as well as by exogenous processes (e.g., erosion and slope movements) whose intensity varies in space and time. Also, the large relief differences support the intensity of ongoing processes. Most dynamic processes are usually triggered by earthquakes or intensive precipitations (during the rainy season or El Niño period) and different processes can influence each other in terms of triggers. It is reasonable to expect that ongoing climate changes as well as deglaciation will influence future dynamic morphological processes.

Druh

C - Kapitola v odborné knize

CEP obor

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OECD FORD obor

10508 - Physical geography

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2024

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název knihy nebo sborníku

Geoenvironmental Changes in the Cordillera Blanca, Peru

ISBN

978-3-031-58244-8

Počet stran výsledku

20

Strana od-do

21-40

Počet stran knihy

299

Název nakladatele

Springer

Místo vydání

Cham

Kód UT WoS kapitoly

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