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Greenland_sulfate.png (394 × 557 pixels, file size: 23 KB, MIME type: image/png)

Description Sulfate concentration in ice core from Central Greenland, accurately dated by counting oxygen isotope seasonal variations. The year 1815 AD was due to the Mt. Tambora eruption, while prior to that is an unknown eruption.
Date
Source Dai, J.; Mosley-Thompson, E.; Thompson, L. G. (1991). "Ice core evidence for an explosive tropical volcanic eruption six years preceding Tambora". Journal of Geophysical Research (Atmospheres) 96 (D9): 17361–17366. Archived from the original on 2012-09-27.
Author myself
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GNU head Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License.
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18 October 2006

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current12:45, 18 October 2006Thumbnail for version as of 12:45, 18 October 2006394 × 557 (23 KB)Indon~commonswiki{{Information |Description= Sulfate concentration in ice core from Central Greenland, accurately dated by counting oxygen isotope seasonal variations. The year 1815 AD was due to the Mt. Tambora eruption, while prior to that is an unkn

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