Nizhne-Koshelevsky New thermal field is located on the watershed between Gremuchiy and Pryamoy brooks in close proximity (300-400 m) to the well-known Nizhne-Koshelevsky thermal anomaly. It was found in 2008 year as a result of vegetation burn on the area of 200 х 200 m and rise of ground temperature up to 100 ºC in the central part of the field. Starting from 2009, the given new formed field has been annually observed (in summer field working period): areal temperature surveyings and lithogeochemical (mercurymetrical) testings of soil-pyroclastic deposits are conducted, their section studies in the central and periphery of the field are carried out, vegetation boundary changes are registered, geophysical works are organized. The change of temperature and geochemical conditions of the thermal field over a period from 2009 to 2013 is also traced. Generalization of findings and regular researches continuation in the area of Nizhne-Koshelevsky New thermal field will make it possible to answer the question about the nature of the given phenomenon.

Ichinsky volcano is the largest volcanic structure of the Sredinny Range of Kamchatka. The manifestation of fumarole activity on the northern slope of the volcano is known since 1956. 64 years after the discovery of the Ledovaya fumarole, it was inspected with a quadrocopter. It was found that the fumarole is located at an altitude of 2725 m and is a large funnel up to 60 m in size, covered with snow in the middle part. In the upper part of the funnel there is a hole in the ice mass 9.8 m in diameter, with vapor-gas clouds rising up to 5–10 m above its edge.. The walls of the ice well are covered with a grayish-yellow fouling of sublimations. The authors believe that the probable temperature of the vapor-gas mixture of fumaroles at the outlet of the volcano rocks is significantly higher than 100° C.