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1 Density of Alae lava and variation with time-Continued Page Introduction _ _ _ _ _ _ __ ___ _ _ _ __ ____ _ _ _ _ _ _ __ __ __ __ _ _ _ _ __ __ __ __ 2 Density and vesicularity  19 Acknowledgments 3 Methods of study 3 Altitude ofthe lake surface 23 Changes in altitude during solidification  24 Drilling ____ __ _ _ _ _ __ ____ __ _ _ _  __ __ __ _ _ __ __ __ __ 3 Changes in horizontal distance during solidification __ 30 Temperature measurements  5 Changes in altitude during further cooling  31 Measurements of the altitude of the lake surface ____ 6 Interpretation of changes in altitude  32 Precipitation and air temperatures 7 Subsidence of the lake surface and calculation of the coefficient of thermal expansion _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 32 Temperatures in the lava lake7 Definition of crust and fluid lava 7 Changes in altitude of the surface during solidification Effect of coolant water on temperatures  11 of the lake _ ___ __ _ _ _ _ __ __ ____ _ _ __ ____ __ __ _ _ _ _ _ _ __ 33 Temperatures in fluid lava below the crust  12 Calculation of the density of fluid lava in the lake 35 Thermal history of the lake   13 The pattern of cooling in three dimensions  37 Maximum temperatures and temperatures at the basal Thermal properties of Alae basalt  40 contact  17 Thermal modeling ____ _ _ _ _ _  __ _ _ _ _  _ _ _ _ _ _ _ _ __ ___ _ 45 Density of Alae lava and variation with time of the altitude of the lake surface 19 Conclusions  48 References cited 49

Cooling and vesiculation of Alae lava lake, Hawaii