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30 May 2006: 8 ). ( 4. 8 b ). = 0 (n-reven), (4 8 c ) and Fnr = t w ' q s ,. , g , , r B B / ( b r - b n ). (,4.9). We again suppress the argument. ... 4.10 b ) N ( - )" 23(nw cosh [)-$ sin ( w cosh inn - &I-) sen(?).

30 May 2006: I n the former case. g ( t , y ) (Bt1-l (B-,O), (3.22). ... For B B 1 l,he penetration depth f L / N is much less than the actual depth H , and the critical height varies inversely with B.

27 Apr 2006: tems. In addition, crystals an d b u b b l es in m ag m as m a y b e distributed so t h at they create stable den- ... G. F. G i b b , C. M. B. H e n d e r s o n , C.

30 May 2006: b P 2 b FIGURE 1. Finite obstacle in seini-infinite, stratified flow. ... The most interesting special cases are given by. A , = 4 h 2 ( A / 2 m ) ( l o g ( 4 h / b ) - 1}OO(b21og(h/b)} (b/hO) (A 7 ) and.

15 Sep 2006: Finally (1) and (4) can be written. d r b 4/3 _,d t b b I b b - b •. Equations (8)-(l 1) describe the heat transfer and melting process ... a). 50 100. b). 100. c). 50 100. TIME (yrs). F I G.

5 Jan 2006: ρs AH, φg =. mg. ρgAH, φl = 1 (φs φg), (1.1a, b, c). ... a) Ballotini in water, (b) KNO3 in solution,(c) KNO3 ballotini in solution.

18 Sep 2006: Sparks: The Fluid Dynamics of a Basaltic M a g m a C h a m b e r. ... The crystals begin to settle, leading to a concentration which increases towards the b o t t o m.

27 Apr 2006: o c k e d b y r u b b l e a n d previous- ly c o o l e d lava. ... p a n d s t o f o r m t h e r u b b l y surface.

30 May 2006: D = au3,/B, (10). 274 H. E. Huppert, J. S. Turner and M. ... of the layer. Hence. where B, is the buoyancy flux at the origin.