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Welcome to Wikipedia!!! First of all, I would like to thank you for visiting Wikipedia and my personal page. I'm a native speaker of English, and love reading fantasy books; may I introduce some to you? The Dragonlance series, Shannara series, and Animorphs are my favourites. Anyway, I hope that Wikipedia will become an even better encyclopedia than it is already.
I just came back from a very long Wikibreak; so I just want to let you Wikipedians know that somewhere out there, I'm still alive. That means you're free to ask me any questions, or contact me about anything (and everything). I'm still open for coaching, so send me a message if you need a coach. If you want someone else for whatever reason, look here. I'm only free on weekends though, so I won't be able to respond to your messages that quickly. And my autograph page is still up and running, so don't hesitate to add your siggie in there! And I have a couple (only a couple, I'm afraid...I'm too lazy to make more =)) of cards that I've made featured here; take a look! Well, that's all I guess. Cheers and a happy new year to you! Zacharycrimsonwolf 08:29, 17 January 2009 (UTC)
Edit: I am no longer active on Wikipedia (as a User, at least) so I'm afraid I can't answer questions from anyone - I suggest that you try looking for an active User around the site if you really need help. When all else fails, moderators, admins, even the Community Portal on your left will work. See you around!
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
An External links section, if any, should always be placed at the end of the article. It should always be spelled that way, never "External Links" or "external links". The term should be used even if there is only one external link.
Sometimes, a user will post a question and forget all about it. It is easy to forget about these unless you keep a record of the questions you posted to refer back to later. One useful method for doing this is to set aside a section of your User page or Talk page, to keep a list of links to your queries. In this list, you can place section links which lead directly to the subheadings (AKA sections) under which you posted your queries.
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