Cavernous Weathering
Cavernous Weathering is a geomorphological weathering process characterized by the development of rock cavities or honeycomb-like voids, typically on vertical or near-vertical rock surfaces, resulting from localized differences in moisture retention and salt crystallization within the rock matrix.
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2017–2026
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UNDERGROUND METEOROLOGY-“What’s the weather underground?”
G. Badino · Acta Carsologica · 2010 · 163 citations · Full text
Salt as an agent in the development of cavernous weathering
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University of Wollongong
Wollongong, Australia
3 h-index
3 publications
173 citations
California Institute of Technology
Pasadena, United States
2 h-index
3 publications
120 citations
Institute of Geology and Geophysics
Beijing, China
2 h-index
7 publications
104 citations
University of Oxford
Oxford, United Kingdom
2 h-index
3 publications
210 citations

University of Ottawa
Ottawa, Canada
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2 publications
78 citations

Carleton University
Ottawa, Canada
2 h-index
2 publications
78 citations

Chinese Academy of Sciences
Beijing, China
2 h-index
7 publications
104 citations

University of Turin
Turin, Italy
1 h-index
1 publications
163 citations
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7 publications · 433 citations
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2 publications · 138 citations
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