Hi! I'm the User 虚ろ長! For those of you who can't read or understand Japanese, too bad!
I'm a friend of User:Hiddenhearts my other account is User:ECH3LON whose kindness has shown us there is good in the world.
I love to work on this website which I will! Uh...keep making this place great!
I'm a good samaritan and i love to help out in debates (especially Articles for Deletion that's one easy way to get started. I LOVE to read, i also love to play videogames
and watch South Park. My favorite bands are Led Zepplin, Journey and All-American Rejects. Oh, and most importantly... I never get tired of helping around this website! =D plz don't steal this...
虚ろ長 00:20, 14 February 2007 (UTC)
| 虚ろ長
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This user is the commander now! Don't order this user around, you civilian!
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This user honestly just doesn't care anymore about what shape the Earth is. Let it go, man.
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 | This user prefers using userboxes to fill up their user page instead of actually writing something useful. |
 | This user was up all night finding userboxes and is now very drowsy. |
 | This user needs more userboxes. MORE, I tell you, more!!! Muhahaha! |
| 1, 2, 3... | This userbox is a test. Please tell this user if you don't see it. |
| This user prefers using userboxes to fill up their user page instead of actually writing something useful. |
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
