User:NerdyScienceDude
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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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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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 |
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