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Taylor, Australian Capital Territory

Suburb of Canberra, Australian Capital Territory From Wikipedia, the free encyclopedia

Taylor is a suburb in Gungahlin, Canberra, Australia. Development of the suburb began in 2017.[citation needed] It is named after magazine publisher Florence Mary Taylor, who was editor of and writer for several Australian building industry journals including the influential Building magazine. The suburb is approximately 4 km from the Gungahlin Town Centre and 16 km from the centre of Canberra and bounded to the south by Horse Park Drive. One Tree Hill lies to the northwest on the border with New South Wales. The suburb is located in north Gungahlin adjacent to the suburbs of Moncrieff, Casey, Jacka and Ngunnawal.

CountryAustralia
Established1991
Elevation
667 m (2,188 ft)
Quick facts Country, State ...
Taylor
Taylor is located in districted Canberra
Taylor
Taylor
Location in Canberra
Coordinates: 35.149°S 149.102°E / -35.149; 149.102
CountryAustralia
StateAustralian Capital Territory
CityCanberra
District
Location
Established1991
Government
 • Territory electorate
 • Federal division
Elevation
667 m (2,188 ft)
Population
 • Total2,220 (SAL 2021)[1]
Postcode
2913
Suburbs around Taylor
Taylor Jacka
Casey Ngunnawal Moncrieff
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History

Until 1991, the suburb Taylor was part of the former 'Gold Creek' a 1,594–hectare rural property with the Gold Creek Homestead at its centre.[2]

Local facilities

A public primary school, Margaret Hendry School, opened in 2019 opposite the Lachlan Kennedy Memorial Park and has capacity for 600 students. It caters to preschool through to year 6 students from the North Gungahlin suburbs of Taylor, Jacka, Moncrieff and Casey (a shared priority enrolment area for Gold Creek School).[3]

Taylor District Playing Fields has 2 rectangle playing fields and is located directly adjacent to Margaret Hendry School.

Geology

The rocks in Taylor are from the late middle Silurian period. Hawkins volcanics green grey dacite and quartz andesite are in the west. The Canberra Formation is separated by a fault in the east side. It consists of slatey shale and mudstone, with north east trending bands of acid volcanics (dacite and andesite).[4]

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