Results 11 to 20 of about 1,006 (66)

Fieldworks at Alaid volcano in 2020, Atlasov island, the Kuriles. Phase 2

open access: yesВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, 2020
The second phase of field work in 2020 on the Alaid Volcano, located on Atlasov Island in the north of the Kuril Island Arc, was carried out on October 2.
Рашидов В.А.   +1 more
doaj   +3 more sources

Erratum to: Petromagnetic and Geochemical Descriptions of Volcanics Discharged by Alaid Volcano, Kuril Islands, in 2015–2016 [PDF]

open access: yesJournal of Volcanology and Seismology, 2021
A. N. Didenko   +5 more
openaire   +2 more sources

To the 90th anniversary of the eruption of the Taketomi side volcano (Atlasov Island, Kuril Island Arc)

open access: yesВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, 2023
The eruption of the unique Taketomi side volcano, located on Atlasov Islandin the northern part of the Kuril island arc, started underwater and ended on land. It happened before people’s eyes and was essentially the formation of a new volcano.
V.A. Rashidov
doaj   +1 more source

Changes in Abiotic Drivers of Green Sea Urchin Demographics following the Loss of a Keystone Predator

open access: yesJournal of Marine Sciences, Volume 2023, Issue 1, 2023., 2023
Sea urchin population demographics can respond to changes in keystone species abundances, with the magnitude of these responses varying depending on environmental influences. In this study, sea urchin populations were surveyed across 15 Aleutian archipelago islands over a 30‐year period to understand how patterns of sea urchin demography (density ...
B. P. Weitzman   +7 more
wiley   +1 more source

Correlations Between Subduction of Linear Oceanic Features and Arc Volcanism Volume Around the Pacific Basin

open access: yesGeochemistry, Geophysics, Geosystems, Volume 23, Issue 12, December 2022., 2022
Abstract Arc volcanoes, created by magma generated from the dehydration of subducting slabs, show great variability in their sizes and along‐arc spatial distributions. In this study, we address a fundamental question, namely, how do subduction zones and volcanic arcs respond to the subduction of “atypical” oceanic lithosphere.
Claudia Adam   +3 more
wiley   +1 more source

ATAKAMIT AS A PRODUCT OF FUMAROLE MINERAL FORMED ON MODERN ON VOLCANOES

open access: yesПроблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского, 2021
The results of electron microscopic, X-ray, IR-spectroscopic and X-ray microprobe studies of atacamite mineralization of fumarole origin on Alaid volcano (Kuril island arc) are discussed.
V. Silaev   +6 more
semanticscholar   +2 more sources

Volcanic Ash versus Mineral Dust: Atmospheric Processing and Environmental and Climate Impacts

open access: yesInternational Scholarly Research Notices, Volume 2013, Issue 1, 2013., 2013
This review paper contrasts volcanic ash and mineral dust regarding their chemical and physical properties, sources, atmospheric load, deposition processes, atmospheric processing, and environmental and climate effects. Although there are substantial differences in the history of mineral dust and volcanic ash particles before they are released into the
Baerbel Langmann   +2 more
wiley   +1 more source

The January 2022 eruption of Hunga Tonga-Hunga Ha’apai volcano reached the mesosphere

open access: yesScience, 2022
Explosive volcanic eruptions can loft ash, gases, and water into the stratosphere, which affects both human activities and the climate. Using geostationary satellite images of the 15 January 2022 eruption of the Hunga Tonga-Hunga Ha’apai volcano, we find
S. Proud, A. Prata, Simeon Schmauß
semanticscholar   +1 more source

Alteration‐Induced Volcano Instability at La Soufrière de Guadeloupe (Eastern Caribbean)

open access: yesJournal of Geophysical Research: Solid Earth, 2021
Volcanoes are unstable structures that deform laterally and frequently experience mass wasting events. Hydrothermal alteration is often invoked as a mechanism that contributes significantly to volcano instability.
M. Heap   +10 more
semanticscholar   +1 more source

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