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 issue48Application of sequential fragmentation/Transport theory to deposits of 1723 and 1963-65 eruptions of Irazú Volcano, Costa Rica: Negative dispersion caseThe Cervantes lava flow geomorfology, Irazú volcano (Costa Rica): description of the Central America´s greater lava flow field author indexsubject indexarticles search
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Revista Geológica de América Central

On-line version ISSN 0256-7024Print version ISSN 0256-7024

Abstract

BRENES, José  and  ALVARADO, Guillermo E.. Application of sequential fragmentation/Transport to deposits of 1723 and 1963-65 eruptions of Irazú Volcano, Costa Rica: Positive dispersion case and fractal model. Rev. Geol. Amér. Central [online]. 2013, n.48, pp.87-98. ISSN 0256-7024.

The Sequential fragmentation/transport theory (SFT), applied to grain size analysis of the deposits from the 1723 and 1963-65 Irazú volcano eruptions, showed an appreciable number of cases with positive dispersion, usually associated to particle aggregation. A new fractal dimension is proposed here to explain them as a secondary fragmentation process. This leads to a new fractal model of volcanic eruptive process, where the Hurst Coefficient and the power law exponent are included. Dispersion values near zero suggest the existence of lava pools. Results deduced from the model agree well with field observations.

Keywords : Sequential fragmentation/Transport; Hurst coefficient; power law exponent; volcanic fractal model; Irazú volcano; Costa Rica.

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