Misty springs are thermal mineral springs on the Chukchi Peninsula . They belong to the territory of the Chukotka region of the Chukotka Autonomous Okrug of Russia .
| Misty Springs | |
|---|---|
| Characteristics | |
| Source type | geothermal spring |
| Water temperature | 55 ° C |
| Debit | 7 l / s |
| Mineralization | 3.2 g / l |
| Location | |
| Is a member of the group | Gilmimleveemsky sources |
| A country |
|
| The subject of the Russian Federation | Chukotka Autonomous Okrug |
| Area | Chukotka District |
They are located in an uninhabited area in a crater-like depression of the left-bank terrace in the upper Gilmimleveem River, near even larger Mechigmen sources [1] . The key site is located at the foot of a chain of gentle hills on a flat bottom of the basin, the eastern side of which is more sloping, and the northern side is steep [2] .
The flow rate of the sources is 7 l / s, the heat transfer is 410 Kcal / s (1.7 MW), the base temperature (deep temperature of hydrothermal formation) is 150-200 ° С.
The chemical composition of water (mg / l) [3] : Na 1000, K 69, Ca 108, Mg 12, Li 4.34.
Misty springs are part of the integrated natural monument "Thermal" [2] .
Notes
- ↑ Wetlands of Russia, vol. IV, (comp. A.V. Andreev). . www.fesk.ru. Date of treatment December 18, 2018. M.: Wetlands International, 2001, ISBN 90-5882-986-3
- ↑ 1 2 Belikovich A.V., Galanin A.V., Afonina O.M., Makarova I.I. Flora of protected areas of Chukotka . - BSI FEB RAS. - Vladivostok, 2006 .-- 260 p.
- ↑ E.A. Wakin. High-temperature terms of Chukotka . - Petropavlovsk-Kamchatsky: Institute of Volcanic Geology and Geochemistry FEB RAS, 2002.