P. D. Cole, E. S. Calder, R. S. J. Sparks, A. B. Clarke, T. H. Druitt, S. R. Young, R. A. Herd, C. L. Harford and G. E. Norton, “Deposits from Dome-Collapse and Fountain-Collapse Pyroclastic Flows at Soufrière Hills Volcano, Montserrat,” In: T. H. Druitt and B. P. Kokelaar, Eds., The Eruption of Soufrière Hills Volcano, Montserrat, from 1995 to 1999, Geological Society of London Memoirs, Vol. 21, 2002, pp. 231-262.

has been cited by the following article:

• TITLE: Pyroclastic Flow from Soufrière Hills Volcano, Montserrat: Solid Block Model

  AUTHORS: Irina Nikolkina, Narcisse Zahibo, Tatiana Talipova, Efim Pelinovsky

  KEYWORDS: Landslide Dynamics, Solid Block Model, Soufrière Hills Volcano

  JOURNAL NAME: International Journal of Geosciences, Vol.2 No.3, August 16, 2011

  ABSTRACT: The solid block model is applied to describe the motion of the pyroclastic flow under the joint action of gravity and Coulomb friction. Special attention is paid to characteristics of the pyroclastic flow generated by Montserrat volcano in likely directions. The critical friction angle of the flow propagation is evaluated empirically. Characteristic parameters of the pyroclastic flow (travel time and impact velocity) are well approximated by linear regressions. Proposed estimations of the parameters of pyroclastic flow are useful for the rough and express evaluation of its characteristics.