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Heat-flow measurements have been made in two holes at Deep Sea Drilling Project Site 465, southern Hess Rise, using a recently developed down-hole temperature probe. From the temperature difference between sub-bottom depths of 86.5 and 172 meters, a heat-flow value of 1.36 HFU (56.7 mW/m) is obtained. This value is nearly the same as the mean value for crustal rocks of the North Pacific basin about 100 m.y. old (the age of the oldest sediments at Site 465).

Down-Hole Temperature Measurements and Heat Flow at Hess Rise, Deep Sea Drilling Project Leg 62