User:BrianY
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This user is no longer active on Wikipedia.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
- Favorite Team: Dodgers
- Interests: Politics, Baseball
- Favorite Trip: Lake Tahoe (yearly)
- Edit Count
- SSP Up to Date: At Daily Digest January 18
| 3,100+ |
 | This user is a participant in WikiProject Baseball. |
| fr-2 | Cet utilisateur peut contribuer avec un niveau intermédiaire en français. |
 | This user is a cat lover. |
| V | This 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. |
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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...
→ We are one people.
Fumarole minerals are minerals that are deposited by fumarole exhalations. They form when gases and compounds desublimate or precipitate out of condensates, forming mineral deposits. They are mostly associated with volcanoes (as volcanic sublimate or fumarolic sublimate), following deposition from volcanic gas during an eruption or discharge from a volcanic vent or fumarole, but have been encountered on burning coal deposits as well. They can be black or multicoloured and are often unstable upon exposure to the atmosphere. This natural-color photomicrograph of fumarole minerals from Mutnovsky, a volcano on the Kamchatka Peninsula in Russia, was taken using a scanning electron microscope. Yellow and red crystals of thallium(I) iodide are visible, with a gradual transition between the two polymorphs. The crystals are located on a substrate of altered rock. This image is 700 micrometres (0.028 in) across on the long side.Photograph credit: Mikhail Zelensky