ALCAROL
Alcarol Karst Gem 凳子
喀斯特是一種獨特的景觀,由水對可溶性岩石的溶解作用形成,例如著名的聯合國教科文組織世界遺產白雲石山脈。
每當酸性水開始分解裂縫附近的基岩表面時,就會發生喀斯特的發展。 發生了數千年的地質過程導致了不尋常的地表和地下特徵,從天坑、豎井、消失的溪流和泉水,到復雜的地下排水系統和允許快速且經常是湍流的水流的洞穴。
Alcarol Stool Karst Gem stool
Karst is a distinctive landscape shaped by the dissolving action of water on soluble rocks like the famous Dolomite mountains, Unesco World Heritage.
The development of karst occurs whenever acidic water starts to break down the surface of bedrock near its cracks. The geological process, occurring over many thousands of years, results in unusual surface and subsurface features ranging from sinkholes, vertical shafts, disappearing streams and springs, to complex underground drainage systems and caves allowing for rapid and often turbulent water flow.
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