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9 Mar 2004: 10. 15. 20. 25. l (cm). BFR. BFR. Figure 5. (a) The drainage of the fluid layer and (b) the depth of the fluid layer within the porousmedium as functions of ... 1 23.3 31 7.2 0.67 46.4 158.32 21.6 64 9.4 0.85 75.2 263.23 20.7 48 9.5 0.77

9 Mar 2004: In addition, during such eruptions magma heating orcooling may also occur9,19,20, especially after input of hot basalticmagma at the base of the chamber18. ... eruptions. Earth Planet. Sci. Lett. 114, 505–516 (1993). 20. Floch, A. &

9 Mar 2004: 1.4. 1.2. 1.00 20 40 60 80 100. t. (a). Vol. ... 1.8. 1.6. 1.4. 1.2. 1.00 5 10 15 20 25 30.

9 Mar 2004: ft 1 20. The volume of the current is conserved during the propagation, which on account of Eqs. ... 1718) and (20) can be expressed as. 2Vt r2NhN 1. 6C2r2N rN02 21.

9 Mar 2004: Melnik and Sparks, 1999; Barmin et al.,2002].[20] These models identify that for volatile unsaturated.

9 Mar 2004: phase diagramis linear T L( S ) 5 m S , where m 5 20.

10 Feb 2004: Last modified: 20 January 2003 by dia. Comments & suggestions, email.

9 Mar 2004: Silver Street, Cambridge CB3 9EW, UK. (Received 9 September 2001 and in revised form 20 December 2001). ... idealized motion, needs some modifications (a reduction of typically 20%)in real circumstances.

9 Feb 2004: 15 and 20 kmalong the ground at velocities of around 100 m s1 (Sparks et al. ... 20 m)pipe held horizontally a few centimetres above a bed of loose sand and silt.

9 Mar 2004: Cur. rent. leng. th. 40%30%20%10%. 0%. Dimensionless time, t. Figure 2. ... ξ,s) = 1 s1(ξ) s22(ξ) , (3.20). F(s) = F0 sF1 s2F2.