Geomorfologické výzkumy na Machu Picchu, Peru.

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F05%3A00000260" target="_blank" >RIV/00025798:_____/05:00000260 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Chapter 4: Geomorphological investigations at Machu Picchu, Peru

Popis výsledku v původním jazyce

Landscape evolution at Machu Picchu is complex. Destructive geomorphologic processes have often followed predispositions by tectonic structure. Besides slope movements, also river erosion and selective mass wasting by weathering and superficial and uderground erosion has been active, there. Large-scale slope movements have seriousy affected mountain morphology. Yet, their present-day activity remains uncertain, in spite, that monitoring time series have shown irreversible movements of the order of 0,1 mm/year at several sites of the archaeological area. Underground erosion by suffosion along tectonically and by the large-scale landslides shattered zones, and uneven settlements of heavy stone buildings on water more saturated grounds are the other potential explanations to those movements. In any case, the occurrence of a large-scale catastrophically rapid slope movement event is improbable within the short time interval of several years, if the present day conditions are maintained.

Název v anglickém jazyce

Chapter 4: Geomorphological investigations at Machu Picchu, Peru

Popis výsledku anglicky

Landscape evolution at Machu Picchu is complex. Destructive geomorphologic processes have often followed predispositions by tectonic structure. Besides slope movements, also river erosion and selective mass wasting by weathering and superficial and uderground erosion has been active, there. Large-scale slope movements have seriousy affected mountain morphology. Yet, their present-day activity remains uncertain, in spite, that monitoring time series have shown irreversible movements of the order of 0,1 mm/year at several sites of the archaeological area. Underground erosion by suffosion along tectonically and by the large-scale landslides shattered zones, and uneven settlements of heavy stone buildings on water more saturated grounds are the other potential explanations to those movements. In any case, the occurrence of a large-scale catastrophically rapid slope movement event is improbable within the short time interval of several years, if the present day conditions are maintained.

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

R - Projekt Ramcoveho programu EK

Rok uplatnění

2005

Kód důvěrnosti údajů

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

Název statě ve sborníku

Landslides. Risk Analysis and Sustainable Disaster Management

ISBN

3-540-28664-0

ISSN

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e-ISSN

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Počet stran výsledku

6

Strana od-do

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Název nakladatele

Springer

Místo vydání

Heidelberg

Místo konání akce

Heidelberg

Datum konání akce

1. 1. 2005

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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