The Behaviour of Cu, Zn, and Pb in Modern Volcanic Processes: Implications for the Genesis of Sulphide Deposits (1991)
Naboko S.I., Glavatskikh S.F. The Behaviour of Cu, Zn, and Pb in Modern Volcanic Processes: Implications for the Genesis of Sulphide Deposits // Volcanology and Seismology. 1991. Vol. 12. № 2. P. 214-240.
The Bezymyannyi, Shiveluch, and St. Helens volcanoes: A comparative revision of their catastrophic eruptions during the 20th century (2015)
Slezin Yu.B. The Bezymyannyi, Shiveluch, and St. Helens volcanoes: A comparative revision of their catastrophic eruptions during the 20th century // Journal of Volcanology and Seismology. 2015. Vol. 9. № 5. P. 289-294. doi:10.1134/S0742046315050073
The Birth of a New Extrusive Dome of the Sheveluch Volcano (Kamchatka) in 2024 According to Continuous Satellite Monitoring in the VolSatView Information System (2024)
Girina O.A., Manevich A.G., Loupian E.A., Melnikov D. V., Nuzhdaev I.A., Uvarov I.A., Romanova I.M., Sorokin A.A., Kramareva L.S., Nuzhdaev A.A. The Birth of a New Extrusive Dome of the Sheveluch Volcano (Kamchatka) in 2024 According to Continuous Satellite Monitoring in the VolSatView Information System // Cosmic Research. 2024. Vol. 62. Vol. Sup. 1. P. S12-S17. https://doi.org/10.1134/S0010952524601099
Annotation
Sheveluch is one of the most active volcanoes in Kamchatka. Its modern edifice includes three main elements: Old Sheveluch, an ancient caldera and Young Sheveluch. On the southeastern slope of Old Sheveluch, there is a group of ancient extrusive domes (from south to north): Sherokhovataya, Krasnaya, Karan, and Sopochka na sklone. Only in the area of the Karan dome are there heated areas with mofets temperature of 70–96°C. After the powerful explosive eruption of the Sheveluch volcano in April 2023, the gas–steam activity of the Karan dome intensified, and a thermal anomaly began to be noted in satellite images of the area of this dome. On April 26, 2024, in a JPSS-1 satellite image at 15:07 UTC, Kamchatkan Volcanic Eruption Response Team scientists discovered a bright thermal anomaly in the area of the Karan dome; that is, they recorded a unique phenomenon on this day: the birth of a new volcanogenic formation – the new lava dome. It was given the name 300 years of the Russian Academy of Sciences. As of June 7, 2024, the size of the new dome was 800 × 500 m and the area of the dome crown was 0.19 km2. The eruption of the new lava dome 300 Years of the Russian Academy of Sciences is continuing.
The Catastrophic Paleolahars of the Elbrus Volcano, Northern Caucasus (1998)
Bogatikov O.A., Melekestsev I.V., Gurbanov A.G., Katov D.M., Puriga A.I. The Catastrophic Paleolahars of the Elbrus Volcano, Northern Caucasus // Doklady Earth Sciences. 1998. Vol. 362. № 7. P. 951-954.
The Composition of Volcanic Ash and the Dynamics of the 2013–2016 Zhupanovsky Volcano Eruption (2018)
Gorbach N.V., Plechova A.A., Manevich T.M, Portnyagin M.V., Philosofova T.M, Samoilenko S.B. The Composition of Volcanic Ash and the Dynamics of the 2013–2016 Zhupanovsky Volcano Eruption // Journal of Volcanology and Seismology. 2018. Vol. 12. № 3. P. 155-171. https://doi.org/DOI: 10.1134/S0742046318030028
Annotation
This paper presents the results from a study of ash compositions that were erupted in 2013–2016.
The juvenile component has been identified in the ejecta using data on the morphology and textural features of ash particles and the composition of volcanic glasses. The data set suggests that the activity of the volcano was phreatomagmatic.
The Elbrus caldera in the northern Caucasus (1998)
Bogatikov O.A., Melekestsev I.V., Gurbanov A.G., Katov D.M., Puriga A.I. The Elbrus caldera in the northern Caucasus // Doklady Earth Sciences. 1998. Vol. 363 A. № 9. P. 1202-1204.
The Eruption of Bezymianny Volcano on August 7, 2001 (2002)
Girina O.A., Ozerov A.Yu., Nuzhdina I.N., Zelenski M.E. The Eruption of Bezymianny Volcano on August 7, 2001 // Abstracts. 3rd Biennial Workshop on Subduction Processes emphasizing the Kurile-Kamchatka-Aleutian Arcs (JKASP-3). Fairbanks. June 2002. 2002. P. 110-111.
The Eruptions of the Northern Group of Volcanoes on Kamchatka in 1988-1989: Seismological and Geodesic Data (1993)
Zharinov N.A., Gorelchik V.I., Zhdanova E.Yu., Andreev V.N., Belousov A.B., Belousova M.G., Gavrilenko V.A., Garbuzova V.T., Demyanchuk Yu.V., Khanzutin V.P. The Eruptions of the Northern Group of Volcanoes on Kamchatka in 1988-1989: Seismological and Geodesic Data // Volcanology and Seismology. 1993. Vol. 13. Vol. 6. P. 649-681.
The Evolution of the 300 years of the RAS lava dome of the Sheveluch volcano (Kamchatka) in 2024-2025 (2025)
Manevich A.G., Girina O.A., Melnikov D.V., Nuzhdaev A.A., Romanova I.M., Loupian E.A., Sorokin A.A., Kramareva L.S., Korolev S.P., Uvarov I.A. The Evolution of the 300 years of the RAS lava dome of the Sheveluch volcano (Kamchatka) in 2024-2025 // Journal of Volcanology and Seismology. 2025. Vol. 19. № S1. P. S63-S71. https://doi.org/10.1134/S0742046325700563
Annotation
The Sheveluch volcano is the northernmost active volcano in Kamchatka. In this work, we describe the activity of the new 300 Years of the RAS lava dome of volcano in 2024–2025. Explosive eruptions of the dome were observed on August 17–18, September 1–2, and November 7–10, 2024: eruptive columns rose up to 9, 8, and 11 km above sea level, respectively, and ash plumes were extended for 2400, 1100, and 3000 km to the east and northeast of the volcano. The results of detailed real-time monitoring of the volcanic eruption are presented using a video surveillance system and various satellite data from The Remote Monitoring of Volcanic Activity in Kamchatka and the Kurile Islands information system (VolSatView, http://kamchatka.volcanoes.smislab.ru).
The Evolutionary Stages and Petrology of the Kekuknai Volcanic Massif Reflecting the Magmatism in the Backarc Zone of the Kuril-Kamchatka Island Arc System. Part II. Petrologic and Mineralogical Features, Petrogenesis Model (2013)
Koloskov A.V., Flerov G.B., Perepelov A.B., Melekestsev I.V., Puzankov M.Yu., Filosofova T.M. The Evolutionary Stages and Petrology of the Kekuknai Volcanic Massif Reflecting the Magmatism in the Backarc Zone of the Kuril-Kamchatka Island Arc System. Part II. Petrologic and Mineralogical Features, Petrogenesis Model // Journal of Volcanology and Seismology. 2013. Vol. 7. № 2. P. 145-169. https://doi.org/10.1134/S0742046313020048
Annotation
Кекукнайский массив сформировался в результате тектоно-магматической деятельности, выразившейся образованием щитообразного вулкана, кальдерной депрессии с сопутствующим внедрением экструзий, и завершившейся интенсивным посткальдерным ареальным вулканизмом. Проведено детальное рассмотрение особенностей минералогического состава пород массива. Использование уже имеющихся и дополнительно выявленных индикаторных возможностей породообразующих минералов позволило восстановить общую картину эволюции магматических расплавов и условия кристаллизации пород (различная флюидонасыщенность-обводненность и окисленность системы). Существенно островодужные или внутриплитные характеристики в составе пород массива проявлены на разных стадиях развития единой флюидно-магматической системы. Декомпрессионная эволюция материнской глубинной базанитовой магмы была реализована появлением в промежуточных очагах дочерних магм трахибазальтового (докальдерный этап развития системы) или гавайитового (ареальный вулканизм) состава. Дальнейшая эманационно-магматическая дифференциация этих расплавов в сочетании с кристаллизационной дифференциации в условиях меняющейся P-T-f02 обстановки и привела к образованию всего многообразия пород Кекукнайского массива.
