Add to ORKGChemical deposits inside evaporite (gypsum, anhydrite and halite) caves are far less common than those developed within limestone or volcanic cavities. Moreover they exhibit a lower scarce mineralogical variability due to several reasons, the most important of which are: 1) calcium sulfate and sodium chloride are by far less reactive than calcium carbonate; 2) evaporite outcrops normally have a low mineralogical variability within the cave recharge areas. Therefore these karst environments were less investigated from this point of view in the past: no general paper exists on speleothems developing in halite and anhydrite caves until present, while the last printed one on gypsum (and anhydrite) karst appeared around 20 years ago. Several min...
none1noCaves are amongst the Earth most important minerogenetic environments and actually over 300 m...
Kenya is one of the few countries in which karst cavities are scarce with respect to volcanic ones, ...
The rocks in which karst systems develop are most commonly composed of carbonate sulphate and chlori...
Chemical deposits inside evaporite (gypsum, anhydrite and halite) caves are far less common than tho...
For many years gypsum karst was considered to contain little of interest from the point of view of c...
Perhaps man’s first motivation to explore caves, beyond using them as shelter, was the search for su...
Perhaps man’s first motivation to explore caves, beyond using them as shelter, was the search for su...
Perhaps man’s first motivation to explore caves, beyond using them as shelter, was the search for su...
Evaporites, including gypsum (or anhydrite) and salt (halite), are the most soluble of common rocks;...
At the beginning of the 20th Century the Naica mine became world renown when the largest gypsum crys...
Caves are among Earth\u27s most important minerogenetic environments and they host over 350 minerals...
Freezing of karst water in caves forces the segregation of solutes, a process of rejection of dissol...
Over the past 15 years several expeditions by French, American and especially Italian cavers have un...
Over the past 15 years several expeditions by French, American and especially Italian cavers have un...
none1noCaves are amongst the Earth most important minerogenetic environments and actually over 300 m...
Kenya is one of the few countries in which karst cavities are scarce with respect to volcanic ones, ...
The rocks in which karst systems develop are most commonly composed of carbonate sulphate and chlori...
Chemical deposits inside evaporite (gypsum, anhydrite and halite) caves are far less common than tho...
For many years gypsum karst was considered to contain little of interest from the point of view of c...
Perhaps man’s first motivation to explore caves, beyond using them as shelter, was the search for su...
Perhaps man’s first motivation to explore caves, beyond using them as shelter, was the search for su...
Perhaps man’s first motivation to explore caves, beyond using them as shelter, was the search for su...
Evaporites, including gypsum (or anhydrite) and salt (halite), are the most soluble of common rocks;...
At the beginning of the 20th Century the Naica mine became world renown when the largest gypsum crys...
Caves are among Earth\u27s most important minerogenetic environments and they host over 350 minerals...
Freezing of karst water in caves forces the segregation of solutes, a process of rejection of dissol...
Over the past 15 years several expeditions by French, American and especially Italian cavers have un...
Over the past 15 years several expeditions by French, American and especially Italian cavers have un...
none1noCaves are amongst the Earth most important minerogenetic environments and actually over 300 m...
Kenya is one of the few countries in which karst cavities are scarce with respect to volcanic ones, ...
The rocks in which karst systems develop are most commonly composed of carbonate sulphate and chlori...