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Cosmogenic Nuclide Dating Of Cave Sediments In The Eastern Alps And Implications For Erosion Rates, Philipp Häuselmann, Lukas Plan, Peter Pointner, Markus Fiebig

International Journal of Speleology

Karstic caves are created by water eroding and corroding rocks that can be dissolved. Since both the spring areas of caves (normally at the valley bottom) as well as the recharge is controlled by superficial processes, the morphology of the cave bears strong links to these influences. Lowering of local base levels promotes the development of horizontal phreatic cave passages at progressively lower elevations, resulting in the formation of multi-level karst systems. Upon the next lowering of base level, these upper systems become fossilized, and sediment trapped within them may remain preserved for millions of years. Dating these sediments gives …