Heat flow from the Earth's interior: Analysis of the global data set¶
Pollack, Hurter, & Johnson. (1993). Heat flow from the Earth's interior: Analysis of the global data set: Analysis of the global data set. Reviews of Geophysics.
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Domain-specific¶
- Volcanism
- Volcanism also operates at planetary scale: large igneous provinces such as the Deccan Traps and Siberian Traps produced flood basalts over areas of millions of square kilometres, injected stratospheric sulfate aerosols that suppressed global temperatures for years to decades, and are linked to mass-extinction events at the Cretaceous–Paleogene and Permian–Triassic boundaries; ongoing mid-ocean ridge volcanism creates the entire oceanic crust, whose conductive and hydrothermal cooling as it ages away from the ridges carries the largest share of heat loss from Earth's interior
This sourceReviews of Geophysics, 1993. A global heat-flow compilation putting Earth's heat loss at about 44 TW, more than half of it through young oceanic lithosphere.
Supported in partVerified against the source
- Volcanism also operates at planetary scale: large igneous provinces such as the Deccan Traps and Siberian Traps produced flood basalts over areas of millions of square kilometres, injected stratospheric sulfate aerosols that suppressed global temperatures for years to decades, and are linked to mass-extinction events at the Cretaceous–Paleogene and Permian–Triassic boundaries; ongoing mid-ocean ridge volcanism creates the entire oceanic crust, whose conductive and hydrothermal cooling as it ages away from the ridges carries the largest share of heat loss from Earth's interior
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