By Marjan Temovski

ISBN-10: 3319245457

ISBN-13: 9783319245454

ISBN-10: 3319374095

ISBN-13: 9783319374093

This thesis addresses karst improvement in a terrain characterised by means of a hugely complicated geological and geomorphological evolution. It tackles the level and complexity of either epigenic and hypogenic karst improvement, in line with morphological analyses of caves, mixed with analyses and datations of cave sediments and their correlation to local geological and geomorphological evolution.

 

Hypogenic karst registered is especially the results of hydrothermal speleogenesis as a result of elevated geothermal gradient in reference to within reach Pliocene-Pleistocene volcanic facilities, with incidence of sulfuric acid speleogenesis and ghost-rock weathering as a result of neighborhood geological or lithological keep an eye on. Epigenic speleogenesis is strongly managed via base point oscillations, with additionally examples of deep phreatic (now fossil) caves hooked up to neighborhood base point upward thrust, and per-ascensum speleogenesis.

 

Another very important discovering is the constraining of the timing of Mariovo Lake draining within the Pleistocene, a massive occasion so as to comprehend the geomorphological evolution in Macedonia, because it ended in the onset of fluvial improvement and incision of valleys, shaping many of the current morphology.

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Evolution of Karst in the Lower Part of Crna Reka River Basin (Springer Theses) by Marjan Temovski


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