Abstract
We have performed fall-experiments with basaltic andesite rock samples from Merapi volcano, using an appa- ratus designed to analyze samples heated up to 850 C. Rel- ative pressure changes during impact and fragmentation of the samples were measured by a pressure transducer. From 200 C, dynamic pressure waves were formed on impact and fragmentation. Peak and duration of the pressure signal, and degree of fragmentation were found to strongly increase with increasing temperature of rock samples. The pressure waves are most likely generated by sudden heating of air forcing it to expand. We propose that the observed pressure changes are analogues to pyroclastic surges that may be generated on impact and fragmentation of large blocks during passage of a pyroclastic flow over a steep cliff. We infer that rock tem- peratures of ca. 400 C are sufficient for this process to oc- cur, a temperature common in pyroclastic flows even in distal reaches.
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