THE KAHST OF GUlLLlMONA MOUNTAIN (RANGES BETICAS)
Abstract
This work considers surface karst features developed in the Sierra Guillimona. The elements and factors that have controlled the evolution and the effectiveness of the contemporary morphoclimatic system are analysed in relation to karst processes. the wole suite of karst forms are present in this lanscape: limestone pavernents. dolines. uvalas and poljes are studied in detail. analysing. classifying. and interpreting their morphogenetic evolution.Downloads
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