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- W2200280184 abstract "Tafoni and gnamma are cavernous weathering phenomena that have been extensively surveyed, discussed, and studied. From delicate, polygonal cells (2–4 mm) to huge circular pits (30 m þ), they develop in a variety of rock substrates, commonly in sandstone (tafoni) and granite (gnamma). Early research on their initiation and development was divisive, but current studies indicate polygenetic, differential weathering from intrinsic factors including hydrolysis, hydration of lithologic constituents, to extrinsic influences like moisture availability, insolation, and salinity. Increasingly, it is believed that complex, feedback cycles are responsible for their sigmoidal rates of development." @default.
- W2200280184 created "2016-06-24" @default.
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- W2200280184 date "2015-01-01" @default.
- W2200280184 modified "2023-10-18" @default.
- W2200280184 title "Tafoni and Other Rock Basins☆" @default.
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- W2200280184 doi "https://doi.org/10.1016/b978-0-12-409548-9.09570-1" @default.
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