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Eos, Transactions American Geophysical Union, 1942
The maps of the Sierra Nevada Region have gained enough detail to individualize steep granite‐structures, some of which must have channelled heat to the surface. MAYO, who mapped 4,000 square miles, 1930–1940, in the High Sierras, found many such structures in the forms of hooks or whorls, the outcrops of steep drag‐folds, successive in time and place.
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The maps of the Sierra Nevada Region have gained enough detail to individualize steep granite‐structures, some of which must have channelled heat to the surface. MAYO, who mapped 4,000 square miles, 1930–1940, in the High Sierras, found many such structures in the forms of hooks or whorls, the outcrops of steep drag‐folds, successive in time and place.
openaire +1 more source
Why the Tongan eruption will go down in the history of volcanology
Nature, 2022Witze Alexandra
exaly
Quaternary Evolution of Ischia: A Review of Volcanology and Geology
Applied Sciences (Switzerland), 2023Gemma Aiello +2 more
exaly
Prospects and pitfalls in integrating volcanology and archaeology: A review
Journal of Volcanology and Geothermal Research, 2020Felix Riede +2 more
exaly