From a mineralogical point of view, Pestera din Valea Rea presents a great interest. Gypsum is unique in what concerns its type of occurrence and abundance. Gypsum speleothems (flower, crystal, rope, snow, hair, cotton, crust and stalagmite) from Pestera din Valea Rea exhibit features never described before in a Romanian cave. The most typical speleothems are those consisting of gypsum, anhydrite and celestite, yet some may include carbonate minerals (calcite, aragonite, magnesite, hydromagnesite, dolomite, rhodochrosite, malachite) and phosphates (brushite, barrandite, bobierrite, vivianite, wavellite). Quartz, periclase, kaolinite, dickite, nacrite and illite have also been identified in various speleothems
The present note provides an updated list of Romanian cave minerals. A recent survey of the mineralo...
Some of the most outstanding hypogenic gypsum speleothems worldwide have been recently discovered in...
Cioclovina Cave hosted an extensive phosphate deposit estimated at over 50,000 m3. About 30,000 m3 ...
From a mineralogical point of view, Pestera din Valea Rea presents a great interest. Gypsum is uniqu...
The Purcăreţ - Boiu Mare Plateau and the southern edge of the Baia Mare Depression, in Sălaj and Mar...
Recent mineralogical investigations carried out in Scarisoara Glacier Cave pointed out the presence ...
The cave of Poiana Vârtop in the NW Bihor Mountains hosts the fourth largest underground perennial g...
Eighteen minerals belonging to eight chemical groups were identified from three caves within Şălitra...
The secondary minerals from Iza Cave result from the interactions of karst water and/or cave atmosph...
This paper presents the mineralization of five medium-size limestone-caves and eleven skarn-hosted c...
The caves from Cerna Valley, southwest Romania, are ideal for mineralogical studies because the reac...
For many years gypsum karst was considered to contain little of interest from the point of view of c...
A number of rare minerals were recently discovered in different caves from Romania. Fifteen of them ...
Some of the most outstanding hypogenic gypsum speleothems worldwide have been recently discovered in...
About 200 gypsum crystals formed within a black clay deposit in Ponoras cave were analyzed with resp...
The present note provides an updated list of Romanian cave minerals. A recent survey of the mineralo...
Some of the most outstanding hypogenic gypsum speleothems worldwide have been recently discovered in...
Cioclovina Cave hosted an extensive phosphate deposit estimated at over 50,000 m3. About 30,000 m3 ...
From a mineralogical point of view, Pestera din Valea Rea presents a great interest. Gypsum is uniqu...
The Purcăreţ - Boiu Mare Plateau and the southern edge of the Baia Mare Depression, in Sălaj and Mar...
Recent mineralogical investigations carried out in Scarisoara Glacier Cave pointed out the presence ...
The cave of Poiana Vârtop in the NW Bihor Mountains hosts the fourth largest underground perennial g...
Eighteen minerals belonging to eight chemical groups were identified from three caves within Şălitra...
The secondary minerals from Iza Cave result from the interactions of karst water and/or cave atmosph...
This paper presents the mineralization of five medium-size limestone-caves and eleven skarn-hosted c...
The caves from Cerna Valley, southwest Romania, are ideal for mineralogical studies because the reac...
For many years gypsum karst was considered to contain little of interest from the point of view of c...
A number of rare minerals were recently discovered in different caves from Romania. Fifteen of them ...
Some of the most outstanding hypogenic gypsum speleothems worldwide have been recently discovered in...
About 200 gypsum crystals formed within a black clay deposit in Ponoras cave were analyzed with resp...
The present note provides an updated list of Romanian cave minerals. A recent survey of the mineralo...
Some of the most outstanding hypogenic gypsum speleothems worldwide have been recently discovered in...
Cioclovina Cave hosted an extensive phosphate deposit estimated at over 50,000 m3. About 30,000 m3 ...