User:Wylve

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This is an old revision of this page, as edited by Wylve (talk | contribs) at 07:32, 27 May 2007. The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

User:Jacklau96/status2

User:Jacklau96/template/Header

Words of Welcome

Welcome to my user page. I joined Wikipedia in September 22, 2006. Feel free to send email and talk to me. If you have any comments, feel free to tell me by leaving a message in my talk page. Click "talk" on the option panel to go to my talk page.

About Me

Real Name: Jack Lau
Age: SECRET
Home(Where do I live): Shatin, Hong Kong
Time Zone: GMT +8 hours
Gender: Male
School: Renaissance College Hong Kong (Year 6)
Hobby: Computer (I used Windows XP) and draw
Favourite Movie: Harry Potter and the Goblet of Fire
Likes: Read, playing computer, draw, editing Wikipedia articles
Dislikes: Smoking, fighting

Awards

User:Jacklau96/Awards

Userboxes

Global

This user's time zone is UTC+8.
This user wants to stop
global warming.


Wikipedia

This user is proud
to be a Wikipedian.
1,000+This user has made more than 1,000 contributions to Wikipedia.
This user is not a Wikipedia administrator but would like to be one someday.


Hobbies

fan-3 This user thinks that Harry Potter and the Goblet of Fire is the best film ever made.
RCTThis user plays RollerCoaster Tycoon.




Education

Template:User Primary School

ARTThis user's favourite subject is Art.

Template:Schoolesf



Computing

This user uses Windows XP.
This user prefers to play games on a PC.
This user uses Google as a primary search engine.
This user uses Gmail as a primary email service.







Picture of the Day

Map of the shoreline of Lake Estancia at three different periods
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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