John Knife

The reason I entered wikipedia? Who knows?
Well, not exactly, my stupid big bro pushed me to enter here. Sb plz tell me what should I do here!!! That 'd be dandy

Hey bro

Come on, iu cant use bad words on da wikipedia here! --Walter Humala 03:49, 21 November 2006 (UTC)

Please don't create hoax pages, like A day at the barn with Hitler. Thanks, Mak (talk) 01:03, 28 November 2006 (UTC) OK PAL, i just thoiught thatr was a real episode

Encouraging vandalism

Please don't. Thanks. --Guinnog 21:41, 7 December 2006 (UTC)

sockpuppet

I, 72.36.251.234, hereby award you with the sockpuppet star. Because dude.. sockpuppetism!

Bob the Builder - Leet

Please do not add nonsense to Wikipedia, as you did to Hitler in popular culture. It is considered vandalism. If you would like to experiment, use the sandbox. Thank you. Danny 23:45, 28 December 2006 (UTC)

sockpuppet?

maybe you mean this user is controlled by my stupid bro, he's a fucking idiot! he even didnt know to type on the keyboard about half a year ago! I'm Daniel, not Walter, and I'm gonna vandalize his page 'cuz he did it on mine I've just realized that.

HAHA! so 72.36.251.234 is Mikalai, an admin who spends the whole day seeking vandalizm or trolling.

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-colour photomicrograph of fumarole minerals from Mutnovsky, a volcano on the Kamchatka Peninsula in Russia, was taken using a scanning electron microscope and colour-enhanced by optical microscopy. 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

Recently featured:

• Sabella spallanzanii
• Lord Kelvin
• The Great Train Robbery

This user's unblock request has been reviewed by an administrator, who declined the request. Other administrators may also review this block, but should not override the decision without good reason (see the blocking policy).

John Knife (block log • active blocks • global blocks • contribs • deleted contribs • filter log • creation log • change block settings • unblock • checkuser (log))

---

Request reason:

Im not a troll, its just I havent found yet a reason for editing here.

Decline reason:

I'm sorry, I can't see any reason to unblock you. You have contributed nothing that I can see and caused a lot of trouble. Sorry. -- Guinnog 00:22, 18 January 2007 (UTC)

---

If you want to make any further unblock requests, please read the guide to appealing blocks first, then use the {{unblock}} template again. If you make too many unconvincing or disruptive unblock requests, you may be prevented from editing this page until your block has expired. Do not remove this unblock review while you are blocked.