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Vog
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==Description== Vog is created when [[volcanic gas]]es (primarily oxides of [[sulfur]]) react with sunlight, [[oxygen]] and [[moisture]]. The result includes [[sulfuric acid]] and other sulfates.<ref>[http://www.epa.gov/air/urbanair/so2/index.html "Sulfur Dioxide"] on US Environmental Protection Agency web site</ref> Vog is made up of a mixture of gases and aerosols which makes it hard to study and potentially more dangerous than either on their own.<ref name=usgs/> Vog, which originates from volcanic vents, differs from [[Laze (geology)|laze]], created when lava enters the ocean.<ref>[http://hilo.hawaii.edu/~nat_haz/vog/media/VogAndLazeSeminar_Abstracts_29July1991.pdf HOW VOG IS MADE: A PHOTOGRAPHIC PERSPECTIVE] {{Webarchive|url=https://web.archive.org/web/20171101215658/http://hilo.hawaii.edu/~nat_haz/vog/media/VogAndLazeSeminar_Abstracts_29July1991.pdf |date=2017-11-01 }}, ''Vog and Laze Seminar'' (July 29, 1991)</ref> The [[Volcanic winter of 536]] has reports of "A dense, dry fog" in the Middle East, China and Europe.<ref name="Ochoa05_p71">{{cite book |last1=Ochoa |first1=George |title=Climate: the force that shapes our world and the future of life on earth |last2=Hoffman |first2=Jennifer |last3=Tin |first3=Tina |publisher=Rodale |year=2005 |isbn=978-1-59486-288-5 |location=Emmaus, Pennsylvania |page=71 |language=en-us}}</ref> [[Image:Vog from Sulfur dioxide emissions.jpg|thumb|[[Sulfur dioxide]] emissions from [[Halemaʻumaʻu]] creates vog.]] [[Image:Hawaiian Vog.jpg|thumb|Volcanic plumes as seen from [[Space Shuttle Atlantis]]]]
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