Water
The first analysis of Biborteni natural mineral water is performed in 1871. Its subject was the BORHEGYI spring and it was conducted in Budapest by chemist MOLNAR JANOS, a member of the Hungarian Society of Natural Sciences.
In the old days, the internal or external curative usage of mineral waters was made empirically, and knowledge about these treatments was most often transmitted orally, occasionally turning into real legends.
But the development of society
There is no source of information for the exact moment when the exploitation of Biborteni mineral water began. By exploitation we mean the systematic bottling and selling of this product on various market. But Molnar Janos speaks about this mineral water and the fitting out of the spring as early as 1871 in his work
The underground water network gathers rain waters passing through the layers of slate and limestone, this way accumulating many mineral elements.
Carbonated water forms in pools located in underground water-bearing layers of volcanic origin. This structure contains a special type of rocks, called basaltoid andesite, which ensure the permanent enrichment of the water with natural
No documents found.
The village of Biborteni is located in the county of Covasna. The Biborteni mineral water pool, considered a genuine underground treasure for centuries, is located within the area of this village, in the gully of the Baraolt river. Located at the Southern foot of the Baraolt Mountains, at the geographic border separating the Baraolt Massif from the Southern Harghita Mountains, the village is some 600 metres above sea level. The Biborteni mineral water pool area is bordered by the Southern Harghita Mountains in the North, the Batani Depression in the East, the Baraolt Mountains in the South and the Baraolt Depression in the West.