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- W4313401083 abstract "According to origin, karst caves are, of course, an underground phenomenon, but in the development of the karst, they frequently appear as surface phenomena that we call “unroofed caves”. Due to the denudation, dissolution and disintegration of carbonate rock and the subsequent lowering of the karst surface, which can be many dozen metres in a million years, underground karst caves are uncovered and with further dissolution can gradually disappear completely. Here we show the frequency, significance and characteristic forms of unroofed caves and place them correctly in the development scheme of the karst cycle. Many years of research of the Classical Karst in Slovenia have shown that unroofed caves are a relatively frequent surface karst form, certainly more frequent that we imagined before expressway construction works in Slovenia’s karst regions uncovered the karst surface. The first attempts to typify their characteristic forms and to explain their formation were born. Our results show the development from old caves to unroofed caves due to the lowering and dissection of the karst surface. Old caves are preserved by sediments, primarily alluvium and flowstone. We present forms of unroofed caves and determine their significance in studying the cavernosity of karst aquifers." @default.
- W4313401083 created "2023-01-06" @default.
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- W4313401083 date "2023-01-01" @default.
- W4313401083 modified "2023-10-07" @default.
- W4313401083 title "Unroofed Cave—An Underground Form on the Karst Surface" @default.
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- W4313401083 doi "https://doi.org/10.1007/978-3-031-16879-6_21" @default.
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