User:Bruxton

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Current time is 22:17:35, 28 May 2024 (UTC)

Very high unreviewed pages backlog: 9244 articles, as of 22:00, 28 May 2024 (UTC), according to DatBot

>Very low pending changes backlog: 2 pages according to DatBot as of 22:15, 28 May 2024 (UTC)

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AwardsThese are my Awards.
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This user has 143 DYK credits.
User:Bruxton/DYK
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This user is the main author of
23 Good Articles
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This user has reviewed 30 Good Article nominations on Wikipedia.
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NPPThis user has reviewed 850 articles during NPP
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This user prefers the Legacy version of the Vector skin to the 2022 version.

This editor is a WikiGnome.
This user has been on Wikipedia for 2 years, 6 months and 2 days.
This user has been a new pages reviewer for 1 year, 11 months, 1 week and 2 days. (verify)
This user has been a pending changes reviewer for 1 year, 2 months, 2 weeks and 6 days. (verify)

RFA

Requests for adminship and bureaucratship update
RfA candidate S O N S % Status Ending (UTC) Time left Dups? Report
DreamRimmer 0 0 0 0 Open 10:02, 4 June 2024 6 days, 11 hours no report

Recently closed RfAs and RfBs (update)
Candidate Type Result Date of close Tally
S O N %
Numberguy6 RfA Closed per WP:SNOW 27 May 2024 5 23 2 18
ToadetteEdit RfA Closed per WP:NOTNOW 30 Apr 2024 0 0 0 0
Sdkb RfA Successful 16 Feb 2024 265 2 0 99

Did you know...

Gyōji with a Pokémon-inspired kimono
Gyōji with a Pokémon-inspired kimono


Picture of the day

Acraea terpsicore
Acraea terpsicore, commonly known as the tawny coster, is a species of butterfly in the Nymphalidae family, the brush-footed butterflies. It is found across eastern Asia from India and Sri Lanka to Singapore, Indonesia and the Maldives and, more recently, Australia. It is small, with a size of 53–64 millimetres (2.1–2.5 in), has leathery wings and is common in grassland and scrub habitats. Acraea terpsicore has a weak fluttery flight and is avoided by most insect predators. This A. terpsicore individual was photographed in Komodo National Park, Indonesia.Photograph credit: Charles J. Sharp

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From tomorrow's featured article

Beulé Gate

The Beulé Gate is a fortified gate leading to the Propylaia of the Acropolis of Athens, Greece. It was constructed largely of repurposed material taken from the 4th-century BCE Choragic Monument of Nikias and integrated into the Post-Herulian Wall, a late Roman fortification built around the Acropolis in the years following the city's sack by the Germanic Heruli people in 267 or early 268 CE. Its construction marked the beginning of a new phase in the Acropolis's use, in which it came to be seen more as a defensive position than a religious sanctuary. During the medieval period, the gate was further fortified, before being built over with a bastion in Ottoman times. The monument was discovered by the French archaeologist Charles Ernest Beulé on 29 May 1852, and excavated in 1852 and 1853. Archaeologists and Greek commentators criticised the aggressive excavation – particularly the use of explosives. In modern times, the gate has served primarily as an exit for tourists from the Acropolis. (Full article...)

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Bomb defusing, photographed by Lander
Bomb defusing, photographed by Lander

In the news (For today)

Mitchell Starc in 2021
Mitchell Starc

On the next day

May 29: Feast day of Saint Paul VI (Catholicism)

Hawthorne Bridge
Hawthorne Bridge
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Tomorrow's featured picture

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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