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Global Impacts of the 1600 Eruption of Peru's Huaynaputina Volcano

2008/04/08 by Kenneth L. Verosub, J. Lippman · 3 citations
Earth and Planetary Sciences · Social Sciences · #Geology and Paleoclimatology Research #Geological and Geochemical Analysis #Pacific and Southeast Asian Studies #Volcano #Unrest #Vulcanian eruption #Social unrest #Stratosphere #Climatology #Geology #Physical geography #Geography #Seismology #Political science

paper · pdf · doi:10.1029/2008eo150001

openalex publication_date 2008/04/08 · openalex created_date 2025/10/10 · openalex updated_date 2026/06/26

Abstract

The human impacts of the 1815 eruption of Tambora volcano in eastern Indonesia are well known. The sulfur injected into the stratosphere by that eruption produced a veil of sunlight‐reflecting sulfate aerosols. The following year, often called the “year without a summer,” was marked by significant global cooling, resulting in crop failures, famine, and social unrest as well as by a broad array of climatic impacts [ Oppenheimer , 2003]. Over the past 10,000 years, there have been many other volcanic eruptions of comparable (and greater) magnitude than Tambora, and at least some of these must have had similar effects. However, Tambora is the only major eruption whose global climatic and human impacts have been comprehensively documented.

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