User:Jorcoga/Sandbox/Old User Page



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About me

Joroga is my name. I registered it on March 17, 2006. I quickly became addicted to Wikipedia (I scored 2046.6019539077613423 on the Wikipediholic Test).
I do make mistakes, just like everyone else, so tell me if I make a mistake. I am very open to critique, I believe that acknowledging mistakes leads to improvement. Also, feel free to contact me whenever you need help or wish to discuss something. You can be rest assured that I will reply as soon as possible.
If you want to know more about me, click here.




Wikipedia Office Tower

Few people know that Wikipedia is in fact a huge skyscraper.
Check the floor directory! Don't look at the hijacked plane on the left.
Stolen from Husond

WP:AIV
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CAT:SPEEDY
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WP:ER
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File:Crude oil pump.jpg WP:VP
WP:BJAODN
WP:BARN
WP:RD

Wikipedia vandalism information
(abuse log)

Level 4
Level 4

Low to moderate level of vandalism

[viewpurgeupdate]


2.38 RPM according to EnterpriseyBot 10:10, 28 June 2024 (UTC)

Fumarole mineral
Fumarole minerals are minerals that are deposited by fumarole exhalations. They form when gases and compounds desublimate or precipitate out of condensates, forming mineral deposits. They are mostly associated with volcanoes (as volcanic sublimate or fumarolic sublimate), following deposition from volcanic gas during an eruption or discharge from a volcanic vent or fumarole, but have been encountered on burning coal deposits as well. They can be black or multicoloured and are often unstable upon exposure to the atmosphere. This natural-color photomicrograph of fumarole minerals from Mutnovsky, a volcano on the Kamchatka Peninsula in Russia, was taken using a scanning electron microscope. Yellow and red crystals of thallium(I) iodide are visible, with a gradual transition between the two polymorphs. The crystals are located on a substrate of altered rock. This image is 700 micrometres (0.028 in) across on the long side.Photograph credit: Mikhail Zelensky
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