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The effect of confining impermeable boundaries on gravity currents in …
www.itg.cam.ac.uk/people/heh/Paper221.pdf6 May 2010: Sd 75 0.24. V 1 20 200 V a 44 0.20 V 2 60 100 V b 75 0.25V 3 40 150 V 4 40 62. -
The Crystallization of Lava Lakes
www.itg.cam.ac.uk/people/heh/Paper118.pdf19 Jul 2010: JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 98, NO. B9, PAGES 15,891-15,901, SEPTEMBER 10, 1993. The Crystallization of Lava Lakes. M. GRAE WORSTER AND HERBERT E. HUPPERT. Institute of Theoretical Geophysics, Department of Applied Mathematics and -
Replenishment of Magma Chambers by Light Inputs
www.itg.cam.ac.uk/people/heh/Paper70.pdf19 Jul 2010: Petrol., 24, 133-165, 1983. Eichelberger, J. C., Vesiculation of mafic magma during replenish- ment of silicic magma reservoirs, Nature, 288, 446-450, 1980. -
Initial advance of long lava flows in open channels
www.itg.cam.ac.uk/people/heh/Paper222.pdf27 Aug 2010: However, variations in fountain height in episode 4, asplotted in figure 1.24 of Wolfe et al. ... the night of 24–25 July 1983,when the flow front divided into two parallel lobes. -
PII: 0022-0248(86)90410-0
www.itg.cam.ac.uk/people/heh/Paper76.pdf19 Jul 2010: Trans. Geotherm.Res. 24 (1985) 25. Roy. Soc. London A310(1984) 511. [19] H.E. -
On heating a stable salinity gradient from below
www.itg.cam.ac.uk/people/heh/Paper31.pdf30 Jun 2010: J. Fluid Mech. (1979), vol. 95, part 3, p p. 431-464. Printed i n Great Britain 43 1. On heating a stable salinity gradient from below. By H E R B E R T E. H U P P E R T A N D P. F. L I N D E N Department of Applied Mathematics and Theoretical -
PII: 0012-821X(86)90188-3
www.itg.cam.ac.uk/people/heh/Paper74.pdf15 Jul 2010: After 24 hours the fluid at the surface and floor had reached compositions of about 17 wt.% and 25 wt.% NaNO, respectively. ... Volcanol. Geotherm. Res. 24, 25-54, 1985. J.S. Turner, Buoyancy Effects in Fluids, Cambridge Uni- versity Press, Cambridge, -
Gravitational and buckling instabilities of a rheologically layered…
www.itg.cam.ac.uk/people/heh/Paper169.pdf19 Jul 2010: η1. )w2(0),. (24). (. 1. k2D3 D. )w1(0) η2. η1. (1. -
Komatiites I: Eruption and Flow by HERBERT E. HUPPERT1 ...
www.itg.cam.ac.uk/people/heh/Paper66.pdf19 Jul 2010: Komatiites I: Eruption and Flow. by HERBERT E. HUPPERT1 AND R. STEPHEN J. SPARKS2. 1 Department of Applied Mathematics and Theoretical Physics, University of Cambridge,Silver Street, Cambridge CB3 9EW. 2Department of Earth Sciences, University of -
Dynamics of viscous grounding lines
www.itg.cam.ac.uk/people/heh/Paper220.pdf6 May 2010: H. t+. q. x= 0 (2.24). to form the nonlinear diffusion equation. ... f (ξ ) dξ = 1, (3.24). to the leading-order front solution (3.21).
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