User:WIZRADICAL

Retired

This user is no longer active on Wikipedia.

This user account is retired as the person wants to make a fresh start. The new account is User:Force Radical

Note:As of 12 February 2018 I have logged in once more to change the name of the current account above –WIZRADICAL (talk) 11:04, 12 February 2018 (UTC)

Disclaimer:This Page is mean to be humorous and serves no encyclopedia purpose!

This Page is being developed and is underconstruction

Welcome! You have finally arrived at the:-

WIZRADICAL HEADQUARTERS, WIKIPEDIA, EARTH, SOLAR SYSTEM, MILKY WAY, LOCAL GROUP,

UNIVERSE

Activity level: User:WIZRADICAL/Status

Take a deep breath Hyper-spatial travel does leave one dizzy...............Have a cuppa of virtual tea....or may be you need a Neutrino Fizzy Delight.........Take seat at the virtual sofa there.......When you are ready buckle up on the sky elevator to go to your desired floor!

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Picture of the day

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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