Retired
This user is no longer active on Wikipedia.
Welcome!
I live in Bishop, California in the Sierra Nevada Mountain range.

Facts:

  • Birth location: Ireland
  • Age: 18
  • Favorite Food: Carrot or Lettuce
  • Favorite Sport: Baseball
  • Interests: Politics, Baseball
  • Favorite Trip: Lake Tahoe (yearly)
  • Edit Count
  • SSP Up to Date: At Daily Digest January 18
3,100+This user has made more than 3,100 contributions to Wikipedia.
fr-2Cet utilisateur peut contribuer avec un niveau intermédiaire en français.
This user is a cat lover.
VThis user is a vegetarian.


This user eats apples.
This user eats bananas.
This user loves oranges.
This user loves to eat pineapples.
This user eats watermelon.
This user loves eating carrots.
This user eats green beans.
This user loves to eat cucumbers.
This user eats potatoes.
This user eats salad.
This user eats spinach.
This user eats candy corn.
This user likes pie.
This user likes Ice cream.
This user is interested in law.
This user enjoys filmmaking.
This user enjoys pottery.
This user is interested in politics.
This user wants to stop
global warming.

Today's motto...
Sarcasm is the language of the devil, for which reason I have long since as good as renounced it.


Nominate one today!

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