Mount Pele, an ecoclimatic gradient generator

dc.contributor.authorJoseph, Philippe
dc.date.accessioned2021-06-28T11:08:30Z
dc.date.available2021-06-28T11:08:30Z
dc.date.issued2013-05-29
dc.description.abstractGenerally, mountains determine the characteristics of particular areas, because of the island phenomenon they cause. However, the geological origins of mountains are multiple and they are located in different climatic regions. Nevertheless, in all aspects they reflect the basic elements of the local biologic unit. The shapes, climates, diverse water resources, biocenoses and the generated soils are the different components that determine, through their dynamic interaction, the “Mountain” ecosystem. Tectonic subduction processes lead to the development of islands such as Martinique, whose basic structure consists of a series of mountains (among them Mount Pele). Like the topographic divisions, the local micro-climates, water courses, different soils (themselves the consequences of the presence of the mountain itself) and successive volcanic eruptions determine, over time, the organization of the diverse vegetal entities.en
dc.formatapplication/pdf
dc.identifier.citationActa Geographica Debrecina Landscape & Environment series, Vol. 7 No. 1 (2013) , 27-41
dc.identifier.eissn1789-7556
dc.identifier.issn1789-4921
dc.identifier.issue1
dc.identifier.jatitleLandsc. environ.
dc.identifier.jtitleActa Geographica Debrecina Landscape & Environment series
dc.identifier.urihttps://hdl.handle.net/2437/317418en
dc.identifier.volume7
dc.languageen
dc.relationhttps://ojs.lib.unideb.hu/landsenv/article/view/2299
dc.rights.accessOpen Access
dc.subjectMartiniqueen
dc.subjectecosystemen
dc.subjectsuccessive processen
dc.subjectclimaxen
dc.subjectvegetation coveren
dc.titleMount Pele, an ecoclimatic gradient generatoren
dc.typefolyóiratcikkhu
dc.typearticleen
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