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9 Mar 2004: flow. Pyroclastic flows can be up toseveral thousands of cubic kilometres in volume, propagating for tens of kilometresfrom the vent of a volcano at speeds over 200 m s1 (Sparks et ... ume. Vmax30. 0t. (b). Vmax. 200 400 600 800 1000. 25.

26 Apr 2006: thickness around day 200 is due toflushing of surface melt water through an artificial bore holeand the creation of a false bottom.

22 Mar 2007: tters 255 (2007) 164–176www.elsevier.com/locate/epsl. Earth and Planetary Science Le. Modelling carbon dioxide accumulation at Sleipner: Implicationsfor underground carbon storage. Mike Bickle a,⁎, Andy Chadwick b, Herbert E. Huppert c, Mark

27 Apr 2006: Fluid Mech. 33 (1968) 183-200. 16 H.E. H u p p e r t and P.F.

12 Jun 2006: We then adapt our code to the configurationof Worster [1]. Since analytical results are obtained in a semi-infinite domain, we impose a very large aspectratio w/h = 200 and choose

24 Apr 2014: year1 (megatonnes CO2 injected per year) since 1996 into the Utsira sandstone, a 200–300-m-thick, highly porous, and permeable reservoir. ... 1,200. 1,300. 1,400. TWTT. (ms). W E. TUTU. BUBU. IHIH. TU.

5 May 2006: Perspex, 1.1 cm thick, with internal lengths and depths of 50 cm 30 cm, 200 cm 22.3 cm and 232.5 cm 40 cm.

27 Apr 2006: Glaciol., 33, 194–200. Eicken, H., H. R. , .

15 Sep 2006: 400. 300. 200. a). BS. 100 2O0 300. TIME (yre). S! ... 100. 400. b). 100 200. TIME (yre). 300 4OO. FIG 5 Variations of (a) temperature, and (b) thickness of the silicic magma layer with time for a 500 m thick sillemplaced

9 Mar 2004: 1125WETTLAUFER ET AL.: SOLIDIFICATION OF LEADS. profile was taken after the buoy had reached the oceanic tem-perature, and each subsequent profile is separated by 200 min.A quantitative analysis of ... The initial profile was taken after the buoy had