The title translates to: "Kacharaltur and Konurtyube Site"

Kacharaltur Area is located on the same left bank of the Yassy River as Kara-Shoro, but 200 meters downstream. At the base of the slope and along the riverbed, there are about half a dozen springs of mineral water and gas emissions. In the most concentrated flows, the water has a mineralization of about 6 g/L, with carbon dioxide content up to 1.88 g/L, otherwise closely resembling the indicators of Kara-Shoro. The flow rate of mineral water here is close to 0.5 L/s.

Konurtyube Area is located on the opposite bank of the river from Kacharaltur and slightly downstream. Here, there are six mineral springs of saline water with a sodium chloride composition and mineralization up to 12.5 g/L and CO2 content exceeding 1 g/L.

As a medicinal or therapeutic table water, this water is not bottled due to its high salt content, but it is widely used as a therapeutic water in spa treatments.

The Kara-Shoro deposit was explored using boreholes without delineating areas, which fully justified itself and allowed for the establishment of underground connections of mineral waters from different sources to the surface. One of the boreholes in the Kacharaltur valley, at a depth of 461 m, penetrated beneath a layer of coal-bearing Jurassic rocks containing UMW at all three previously discussed sites, revealing Silurian limestones; from the contact zone of these limestones and the overlying Mesozoic deposits, a flow of sodium chloride carbonated water with a dry residue of more than 40 g/L was obtained. A slightly lower mineralization, but still brine concentration, was identified when testing borehole No. 6 near the Kara-Shoro springs at a depth of 170 m (35.5 g/L). These facts suggest that the "absolute record" of mineralization of carbonated waters in the deposit has likely not yet been reached, but the results obtained already indicate the high potential of Kara-Shoro to meet a wide variety of consumer demands: there is almost fresh carbonated water, brine, and all imaginable concentrations in between.