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- W2498265887 abstract "Volcanic landforms on the Earth range are shapes and sizes from tiny scoria cones to enormous flood basalt or ignimbrite plateaux. Controls on the final volcanic landform include magma composition and volume, tectonic environment, nature of the crust, and posteruption erosion. Primary volcanic landforms (pre-erosion) can be divided into polygenetic and monogenetic volcanoes. The former include composite, shield, and caldera volcanoes; the latter include mafic minor centers such as scoria and spatter cones, tuff rings and cones, maars and kimberlites, as well as silicic minor centers such as lava domes and coulées. The most obvious volcanic landforms at the planetary scale are spatially, temporally, and magmatically connected volcanic provinces, such as volcanic fields, volcanic arcs, and large igneous provinces. These may contain all of the individual polygenetic and monogenetic volcanic landforms regardless of tectonic environment, providing strong evidence for universal primary controls on the character of Earth's volcanic landforms." @default.
- W2498265887 created "2016-08-23" @default.
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- W2498265887 date "2015-01-01" @default.
- W2498265887 modified "2023-10-14" @default.
- W2498265887 title "Primary Volcanic Landforms" @default.
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- W2498265887 doi "https://doi.org/10.1016/b978-0-12-385938-9.00015-8" @default.
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