This user may have left Wikipedia. NerdyScienceDude has not edited Wikipedia since September 4, 2012. As a result, any requests made here may not receive a response. If you are seeking assistance, you may need to approach someone else. |
Please note that I'm not very active. I am very busy in real life. I will pop in every once in a while to make a handful of minor edits every now and then. |
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For several years now I have found several useful facts from Wikipedia. As a result I decided that I should help edit it. My name is NerdyScienceDude. I have been active on Wikipedia since January 2009 as an IP address. I created my account on December 3, 2009. Since then I have been granted
rollback and
reviewer rights. I enjoy editing articles about
German U-boats,
NASCAR,
Skyscrapers,
Macintosh and
Apple Inc.,
iOS,
New Mexico, and
Scouting. I'm a dedicated
vandal fighter as well; I use
Twinkle and
igloo to aid my vandal-fighting and CSD tagging. I also use tools such as
Friendly,
Nice,
Hotcat,
Advisor.js, and
dashes.js. I also hang out at
WP:ANI,
WP:AIV,
WP:UAA,
WP:SPI,
WP:RFA,
WP:RPP, as well as clerking
WP:CHU sometimes. Before I got my Wikipedia account, I edited under the IPs
98.230.214.136,
68.35.20.151, and
69.254.153.143. I would find the
administrator tools useful in my work, and I hope to become one in the future. I made my first edit ever on January 18, 2009. It was
this edit to
List of tallest buildings in the world using the 98. IP address.
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Guestbook
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Content creations
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ArticlesEnglish
Simple EnglishRedirects
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Image gallery
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DYK's
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GA's
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GA Reviews
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Picture of the Day
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Lake Estancia was a
prehistoric body of water in the
Estancia Valley, in the center of the U.S. state of
New Mexico. Mostly fed by creek and
groundwater from the
Manzano Mountains, the lake had diverse fauna, including
cutthroat trout. It appears to have formed when a river system broke up. It reached a maximum water level (highstand) presumably during the
Illinoian glaciation and subsequently fluctuated between a desiccated basin and fuller stages. Wind-driven erosion has excavated depressions in the former lakebed that are in part filled with
playas (dry lake beds). The lake was one of several
pluvial lakes in southwestern North America that developed during the late
Pleistocene. Their formation has been variously attributed to decreased temperatures during the
ice age and increased precipitation; a shutdown of the
thermohaline circulation and the
Laurentide Ice Sheet altered atmospheric circulation patterns and increased precipitation in the region. The lake has yielded a good
paleoclimatic record. This map shows the shoreline of Lake Estancia at three different periods: early Estancia (1,939 m / 6,362 ft above sea level), late Estancia (1,897 m / 6,224 ft), and "Lake Willard" (1,870 m / 6,135 ft). Present-day populated places, county boundaries and roads are overlaid on the map for identification.Map credit:
Tom Fish
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RFA report
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Funny stuff
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Signature evolution
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Special thanks
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One of the great things about being on Wikipedia is meeting and co-operating with so many people. I would like to thank the following users for the help they have given me while editing Wikipedia...
User page vandalism reverters |
This is a Wikipedia
user page. This is not an encyclopedia article or the talk page for an encyclopedia article. 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 whom this page is about may have no personal affiliation with any site other than Wikipedia. The original page is located at https://en.wikipedia.org/wiki/User:NerdyScienceDude. |