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The Ginkgo basalt was examined over its 500 km (310 mi) flow path from a Ginkgo flow feeder dike near Kahlotus, Washington to the flow terminus in the Pacific Ocean at Yaquina Head, Oregon.
The basalt had an upper melting temperature of 1095 ± 5 °C and a lower temperature to 1085 ± 5 °C; this indicates that the maximum temperature drop along the Ginkgo flow was 20 °C.
An abrupt transition to shield volcanic flooding took place in the mid-Miocene.
These plumes are much more focused than the upwelling observed with large-scale plate-tectonics circulation.We provide the ice-breakers for you and turn it into a game!
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