Landform instability and land-use dynamics in tropical high mountains, Central Mexico
Autor: | Carlos Arredondo-León, Arturo García-Romero, José Fernando Aceves-Quesada |
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Rok vydání: | 2012 |
Předmět: |
Hydrology
Global and Planetary Change geography geography.geographical_feature_category Land use Landform Geography Planning and Development Fluvial Geology Structural basin Alluvial plain Deforestation Physical geography Drainage density Mountain range Nature and Landscape Conservation Earth-Surface Processes |
Zdroj: | Journal of Mountain Science. 9:414-430 |
ISSN: | 1993-0321 1672-6316 |
DOI: | 10.1007/s11629-009-2307-5 |
Popis: | This investigation is an analysis of the influence of landform instability on the distribution of land-use dynamics in a hydrographical basin, located in the Mexican Volcanic Belt mountain range (central Mexico), currently affected by substantial changes in land use and deforestation. A landform map was produced, in addition to seven attribute maps – altimetry, drainage density, slope, relief energy, potential erosion, geology and tectonics – which were considered as factors for determining landform instability through Multi-criteria Evaluation Analysis. Likewise, the direction and rhythm of land-use dynamics were analyzed in four dates – between 1976 and 2000 – and cross tabulations were made between them, in order to analyze the trends and processes of land-use dynamics. Afterwards, the databases obtained were cross tabulated with the landform variables to derive areas, percentages and correlation indices. In the study area, high-instability landforms are associated with most ancient volcanic and sedimentary landforms, where high altitude, drainage density, slope and potential to develop gravitational and fluvial processes are the major factors favouring a land-use pattern, dominated by the conservation of extensive forest land, abandonment of human land use and regeneration of disturbed areas. In contrast, low-instability landforms correspond to alluvial plains and lava hills covered by pyroclasts, where low potential erosion to develop fluvial processes, added to water and soil availability and accessibility, have favoured a land-use pattern dominated by the expansion of agroforestry plantations and human settlements, showing a marked trend towards either intensification or permanence of the current land use and with little abandonment and regeneration. |
Databáze: | OpenAIRE |
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