The 1935‒2024 Summit Eruptions of the Klyuchevskoy Volcano

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
O. A. Girina
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Abstract

Klyuchevskoy is one of the most powerful active basaltic volcanoes in the world. Information about its eruptions has been known since 1697. This paper describes the summit eruptions of the volcano from 1935 to 1999, and analyzes such eruptions from 1935 to 2024. Between 1935 and 2024 30 summit eruptions occurred: 11 explosive eruptions lasting from 6 to 1110 days and 19 explosive–effusive eruptions lasting from 26 to 1100 days. It was found that paroxysmal phases of eruptive events with ash ascent to the maximum height (15 km above sea level) are characteristic only of explosive–effusive eruptions of the volcano. It was noted that paroxysmal phases of eruptions were observed, as a rule, 6–15 days or 1–2.5 months (rarely 2 days or 7 months) before their end, i.e., an increase in the power of ash ascent from the volcanic crater in some cases led to the emptying of the magma reservoir (for example, the eruption of 1994) and in other cases to the rise of new portions of lava to the daylight surface (for example, the eruptions of 1944 and 1987–1990).

Abstract Image

1935年至2024年克柳切夫斯基火山喷发
克柳切夫斯科伊火山是世界上最活跃的玄武岩火山之一。自1697年以来,人们就知道了有关它喷发的信息。本文描述了1935年至1999年的火山喷发,并对1935年至2024年的火山喷发进行了分析。1935年至2024年间,发生了30次山顶喷发:11次爆炸性喷发持续了6至1110天,19次爆炸性喷发持续了26至1100天。研究发现,火山灰上升到最高高度(海拔15公里)的爆发事件的阵发性阶段仅是火山爆发性喷发的特征。是指出,观察阵发性喷发阶段,作为一个规则,6 - 15天或1 - 2.5个月(很少2天或7个月)前结束,也就是说,增加灰的力量崛起的火山坑在某些情况下导致放空水库的岩浆的喷发(例如,1994)和在其他情况下崛起的新部分日光熔岩的表面(例如,1944年和1987 - 1990年的火山喷发)。
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来源期刊
Journal of Volcanology and Seismology
Journal of Volcanology and Seismology 地学-地球化学与地球物理
CiteScore
1.50
自引率
28.60%
发文量
27
审稿时长
>12 weeks
期刊介绍: Journal of Volcanology and Seismology publishes theoretical and experimental studies, communications, and reports on volcanic, seismic, geodynamic, and magmatic processes occurring in the areas of island arcs and other active regions of the Earth. In particular, the journal looks at present-day land and submarine volcanic activity; Neogene–Quaternary volcanism; mechanisms of plutonic activity; the geochemistry of volcanic and postvolcanic processes; geothermal systems in volcanic regions; and seismological monitoring. In addition, the journal surveys earthquakes, volcanic eruptions, and techniques for predicting them.
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