Вулкан Тауншиц. Библиография
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Braitseva O.A., Ponomareva V.V., Melekestsev I.V., Sulerzhitskiy L.D., Pevzner M.M. Holocene Kamchatka volcanoes. 2002.
Girina O.A., Gordeev E.I., Melnikov D.V., Manevich A.G., Nuzhdaev A.A., Romanova I.M. The 25 Anniversary Kamchatkan Volcanic Eruption Response Team // 10th Biennual workshop on Japan-Kamchatka-Alaska subduction processes (JKASP-2018). Petropavlovsk-Kamchatsky, Russia, August 20-26. // 10th Biennual workshop on Japan-Kamchatka-Alaska subduction processes (JKASP-2018). Petropavlovsk-Kamchatsky: IVS FEB RAS. 2018. P. 80-82.
Global Volcanism Program. Volcanoes of the World, v. 4.11.0 (08 Jun 2022). 2013. doi: 10.5479/si.GVP.VOTW4-2013.
   Аннотация
The Volcanoes of the World database is a catalog of Holocene and Pleistocene volcanoes, and eruptions from the past 12,000 years.
Ponomareva V.V., Churikova T., Melekestsev I.V., Braitseva O.A., Pevzner M., Sulerzhitskii L. Late Pleistocene-Holocene Volcanism on the Kamchatka Peninsula, Northwest Pacific Region / Volcanism and Subduction: The Kamchatka Region. Washington, D. C.: American Geophysical Union. 2007. Vol. 172. P. 165-198. doi: 10.1029/172GM15.
   Аннотация
Late Pleistocene-Holocene volcanism in Kamchatka results from the subduction of the
Pacific Plate under the peninsula and forms three volcanic belts arranged in en echelon manner
from southeast to northwest. The cross-arc extent of recent volcanism exceeds 250 km and
is one of the widest worldwide. All the belts are dominated by mafic rocks. Eruptives with
SiO2>57% constitute ~25% of the most productive Central Kamchatka Depression belt and
~30% of the Eastern volcanic front, but <10% of the least productive Sredinny Range belt.
All the Kamchatka volcanic rocks exhibit typical arc-type signatures and are represented
by basalt-rhyolite series differing in alkalis. Typical Kamchatka arc basalts display a strong
increase in LILE, LREE and HFSE from the front to the back-arc. La/Yb and Nb/Zr increase
from the arc front to the back arc while B/Li and As, Sb, B, Cl and S concentrations decrease.
The initial mantle source below Kamchatka ranges from N-MORB-like in the volcanic front
and Central Kamchatka Depression to more enriched in the back arc. Rocks from the Central
Kamchatka Depression range in 87Sr/86Sr ratios from 0.70334 to 0.70366, but have almost
constant Nd isotopic ratios (143Nd/144Nd 0.51307–0.51312). This correlates with the highest
U/Th ratios in these rocks and suggest the highest fluid-flux in the source region.
Holocene large eruptions and eruptive histories of individual Holocene volcanoes have been
studied with the help of tephrochronology and 14C dating that permits analysis of time-space
patterns of volcanic activity, evolution of the erupted products, and volcanic hazards.
Ponomareva Vera V., Melekestsev Ivan V., Dirksen Oleg V. Sector collapses and large landslides on Late Pleistocene–Holocene volcanoes in Kamchatka, Russia // Journal of Volcanology and Geothermal Research. 2006. Vol. 158. № 1-2. P. 117-138. doi:10.1016/j.jvolgeores.2006.04.016.
   Аннотация
On Kamchatka, detailed geologic and geomorphologic mapping of young volcanic terrains and observations on historical eruptions reveal that landslides of various scales, from small (0.001 km3) to catastrophic (up to 20–30 km3), are widespread. Moreover, these processes are among the most effective and most rapid geomorphic agents. Of 30 recently active Kamchatka volcanoes, at least 18 have experienced sector collapses, some of them repetitively. The largest sector collapses identified so far on Kamchatka volcanoes, with volumes of 20–30 km3 of resulting debris-avalanche deposits, occurred at Shiveluch and Avachinsky volcanoes in the Late Pleistocene. During the last 10,000 yr the most voluminous sector collapses have occurred on extinct Kamen' (4–6 km3) and active Kambalny (5–10 km3) volcanoes. The largest number of repetitive debris avalanches (> 10 during just the Holocene) has occurred at Shiveluch volcano. Landslides from the volcanoes cut by ring-faults of the large collapse calderas were ubiquitous. Large failures have happened on both mafic and silicic volcanoes, mostly related to volcanic activity. Orientation of collapse craters is controlled by local tectonic stress fields rather than regional fault systems.

Specific features of some debris avalanche deposits are toreva blocks — huge almost intact fragments of volcanic edifices involved in the failure; some have been erroneously mapped as individual volcanoes. One of the largest toreva blocks is Mt. Monastyr' — a ∼ 2 km3 piece of Avachinsky Somma involved in a major sector collapse 30–40 ka BP.

Long-term forecast of sector collapses on Kliuchevskoi, Koriaksky, Young Cone of Avachinsky and some other volcanoes highlights the importance of closer studies of their structure and stability.
Siebert L., Simkin T., Kimberly P. Volcanoes of the World. Berkeley: University of California Press. 2010. 568 p.
   Аннотация
This impressive scientific resource presents up-to-date information on ten thousand years of volcanic activity on Earth. In the decade and a half since the previous edition was published new studies have refined assessments of the ages of many volcanoes, and several thousand new eruptions have been documented. This edition updates the book's key components: a directory of volcanoes active during the Holocene; a chronology of eruptions over the past ten thousand years; a gazetteer of volcano names, synonyms, and subsidiary features; an extensive list of references; and an introduction placing these data in context. This edition also includes new photographs, data on the most common rock types forming each volcano, information on population densities near volcanoes, and other features, making it the most comprehensive source available on Earth's dynamic volcanism.
VONA/KVERT Information Releases. 2005.
Volcano observatory notification to aviation (VONA/KVERT). 2011.
Апродов В.А. Вулканы. М.: Мысль. 1982. 367 с.
   Аннотация
Справочник содержит характеристику около трех тысяч вулканов земного шара, сгруппированных по вулканическим поясам и другим районам проявления вулканизма. Этим поясам и районам предшествует их общая геолого-географическая характеристика. Сведения о вулканах включают географическое положение, морфологию, геологическую структуру, активность и т.д. Книга рассчитана не только на специалистов, но и на более широкий круг читателей.
Гирина О.А., Лупян Е.А., Сорокин А.А., Мельников Д.В., Романова И.М., Кашницкий А.В., Уваров И.А., Мальковский С.И., Королев С.П., Маневич А.Г., Крамарева Л.С. Комплексный мониторинг эксплозивных извержений вулканов Камчатки / Отв. ред. Гирина О.А. Петропавловск-Камчатский: ИВиС ДВО РАН. 2018. 192 с.
   Аннотация
В монографии приведены различные данные о вулканах Камчатки, описаны возможности их изучения на основе комплексного использования методов и технологий дистанционного зондирования, наземных наблюдений и численного моделирования. Значительное внимание уделено вопросам построения и применения информационных систем, обеспечивающих сегодня оперативный мониторинг и исследования вулканической активности, которые в последние годы совместно разрабатываются и развиваются специалистами Института вулканологии и сейсмологии ДВО РАН (Петропавловск-Камчатский), Института космических исследований РАН (Москва), Вычислительного центра ДВО РАН (Хабаровск) и Дальневосточного филиала НИЦ Планета (Хабаровск). Приведены результаты комплексных исследований эксплозивных извержений вулканов, а также потенциальная опасность действующих вулканов Камчатки для населения и авиации, полученные учеными ИВиС ДВО РАН, в том числе, с помощью представленных в монографии новых методов, технологий и систем.