Frustrated by the comments, edits, and reverts of another user? Remember, behind that sig line is another human being, just like you! And just like you, that person wants to see his or her ideas come to life on Wikipedia.
If you feel yourself getting angry, hurt, or frustrated, explain yourself in a reasonable way and politely ask that others involved in the conversation do the same. But do not expect everyone to agree with you. Differences of background and opinion are part of what makes Wikipedia so great!
To add this auto-randomizing template to your user page, use{{totd-random}}
Always good to peek into the future . . .
Tomorrow's featured article
The Mount Edziza volcanic complex (MEVC) is a group of volcanoes and associated lava flows in northwest British Columbia, Canada. Located on the Tahltan Highland, the MEVC has a broad, steep-sided lava plateau; its highest summit is 2,786 metres (9,140 feet). Its volcanoes formed over the last 7.5 million years during five cycles of magmatic activity which spanned four epochs; the most recent eruptions took place in the last 11,000 years. Current activity occurs in the form of hot springs. The MEVC has warm summers and cold, snowy winters; snow and ice remain on the highest peaks year-round. Indigenous peoples have lived adjacent to the MEVC for thousands of years. Historically, the local Tahltan people used volcanic glass from the MEVC to make tools and weaponry. Animal species such as birds, rodents, bears, sheep, goats, moose and caribou inhabit the area. A large provincial park dominates the MEVC, which can only be accessed by aircraft or by a network of footpaths. (Full article...)
