Hello everyone, I'm Minorax. I've been editing the English Wikipedia for slightly over 6 years now and usually patrol Special:NewPages and find files that can be moved to Commons.
As a global sysop, I patrol small wikis and help out with administrative stuff there, typically finding x-wiki socks and reverting vandalism. For a list of other user rights, see m:User:Minorax/matrix.
If you have any queries or require assistance on wikis that have the GS-toolset enabled, do not hesitate to contact me.
EN-5
This user has professional knowledge of English.
ZH-5
这位用户的中文达到专业水平。
KO-1
이 사용자는 한국어를 조금 할 수 있습니다.
MS-1
Pengguna ini memiliki kemahiran asas dalam bahasa Melayu.
FR-1
Cet utilisateur dispose de connaissances de base en français.
NAN-2
Chit-ê iōng-chiá tha̍k-siá Bân-lâm-gú ê lêng-le̍k sī tiong-kip.
Portrait of Charles Marcotte (also known as Marcotte d'Argenteuil) is an 1810 oil-on-canvas painting by the French Neoclassical artist Jean-Auguste-Dominique Ingres, completed during the artist's first stay in Rome. It depicts the eponymous Charles Marcotte (1773-1864), who was a long-term friend and supporter of Ingres and commissioned the work initially as a gift for his mother. When the portrait was painted, Marcotte served as inspector general for waters and forests in Napoleonic Rome. In the painting, he stands against a plain grey-green background, leaning against a table draped with a red cloth. His stiff, starched white and yellow neck collar appears tight and restrictive. Marcotte did not like the final painting, finding it too stern, and it remained in his possession until his death. It is now in the collection of the National Gallery of Art in Washington, D.C., United States.
Tseax Cone is a small volcano in the Nass Ranges of the Hazelton Mountains in northwestern British Columbia, Canada. It has an elevation of 609 metres (1,998 feet) and lies within an east–west valley through which a tributary of the Tseax River flows. The volcano consists of two nested structures and was the source of four lava flows that descended into neighbouring valleys. A secondary eruptive centre lies just north of Tseax Cone on the opposite side of Melita Lake. It probably formed simultaneously with Tseax Cone; both were formed by volcanic activity sometime in the last 800 years. The exact timing of volcanism at Tseax Cone has been a subject of controversy due to there being no direct written accounts. There is also controversy over whether the volcano was formed during one or more distinct episodes of eruptive activity. The single eruptive episode hypothesis has been proposed by researchers as early as 1923 whereas a multi-eruption hypothesis was proposed in 1978. (Full article...)
.svg?lang=en){kind=logo}
Welcome!
«※¦Minorax¦※»
Talk
Contributions
User logs
Email
CentralAuth
