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136 A. Pittari et al.

ACKNOWLEDGEMENTS

This study draws from the Ph.D. thesis of A. Pittari, supported by an Australian Postgraduate Award
Scholarship and Monash University Small Grant Research Funds to R. Cas, and is part of a
collaborative international Tenerife Research Program led by J. Martı ´. We appreciate the support
provided by the School of Geosciences, Monash University during this study. J. Wolff, H. Nichols
and P. Larson were supported by National Science Foundation grant EAR-0001013. We thank
R. Sulpizio and S. Self for their helpful reviews.

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