Hi. I'm Bratsche. Some call me Ben. You can try either; I'll get back to you after the beep.
I'm a student, who likes to read and fix mistakes. Wikipedia just fulfills my editorial cravings.
Since I don't have much in-depth knowledge of any one subject, but rather a mind full of trivia, I'm on a personal mission to destroy vandalism, delete nonsense and do basic janitorial work with my mop.
By the way, Bratsche means viola in German, my musical instrument of choice
Musicians: Why don't you leave me a good viola joke... :)
Contributors to the playful punishment of violists:
"Imagine a world in which every single person on the planet is given free access to the sum of all human knowledge. That’s what we’re doing." -28 Jul 2004
"Userboxes of a political or, more broadly, polemical, nature are bad for the project." -21 Jan 2006
"... [T]he number of userboxes, and in particular the number of very problematic userboxes, has exploded. I think this is seriously Not Good For Our Loving Little Community." -15 Feb 2006
Est omnino difficile iudicare inclusionis meritum cuiusdam rei in encyclopædia cum ratio sciendi quid populi referat incerta sit, sed nihilominus aliquid encyclopædiam dedecet
It is generally difficult to judge the worthiness of a particular topic for inclusion in an encyclopedia considering that there is no certain way to know what interests people, but some topics nevertheless are not fit for an encyclopedia.
This motto reflects the desire of these Wikipedians to be reluctant, but not entirely unwilling, to remove articles from Wikipedia.
Trou au Natron is a volcanic caldera in the Tibesti Massif in northern Chad. The volcano is extinct, and it is unknown when it last erupted. Trou au Natron is located just south-east of Toussidé, the westernmost volcano of the Tibesti Mountains. The caldera has an irregular diameter of approximately 6 to 8 kilometres (4 to 5 miles) and is up to 1,000 metres (3,300 ft) deep. Because of its irregular shape, it has been theorized that the caldera was formed as a result of multiple massive explosions, each of which deepened the enormous pit. Its exact period of formation is unconfirmed, although a Pleistocene formation has been suggested. Much of the surface of the caldera is lined with a white crust of carbonate salts such as sodium carbonate and natrolite, known as natron, leading to the caldera's name, literally 'hole of natron' in French. This crust is sometimes known as the Tibesti Soda Lake. Both the slopes and the floor of the caldera contain thick layers of fossilized aquatic gastropods and diatoms, indicating that it was once home to a deep lake. This satellite image of Trou au Natron was taken in 2008 from the International Space Station, at an altitude of around 352 kilometres (219 miles). The white crust can be seen at the bottom of the caldera.Photograph credit: NASA
For helping clean up the talk section of the Pope Benedict XVI article, here is the Wikimedal for Janitoral Services. Zscout370 18:02, 20 Apr 2005 (UTC)
In recognition of your persistent dedication to the community on WP:BAP, I hereby award you with The Barnstar of Diligence - Sango123 16:53, Jun 23, 2005 (UTC)
To Bratsche, for going above and beyond when I asked for help--Shanel 22:52, 13 September 2005 (UTC)
I think you deserve this for beating me in reverting to vandalise pages I hearby reward u the RickK anti vandalism award --JAranda | yeah 03:06, 11 October 2005 (UTC)
For all the work you have done. Molotov (talk) 21:36, 13 October 2005 (UTC)
If you find this page on any site other than Wikipedia, you are viewing a mirror site. Be aware that the page may be outdated, and that the user this page belongs to may have no personal affiliation with any site other than Wikipedia itself. The original page is located at http://en.wikipedia.org/wiki/User:Bratsche/User2.
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Svjetlost building.jpg
For helping clean up the talk section of the Pope Benedict XVI article, here is the Wikimedal for Janitoral Services. Zscout370 18:02, 20 Apr 2005 (UTC)
To Bratsche, for going above and beyond when I asked for help--Shanel 22:52, 13 September 2005 (UTC)
