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・ Theodorus Priscianus
・ Theodorus Schrevelius
・ Theodorus the Atheist
・ Theodorus van Kooten
・ Theodorus W. Brevard
・ Theodorus Willem van Lidth de Jeude
・ Theodosia
・ Theodosia (genus)
・ Theodosia Ada Wallace
・ Theodosia and the Serpents of Chaos
・ Theodosia Arm
・ Theodosia Burr Alston
・ Theodosia Formation
・ Theodosia Inlet
・ Theodosia Meade, Countess of Clanwilliam
Theodore, Australian Capital Territory
・ Theodore, Philippa, and Companions
・ Theodore, Queensland
・ Theodore, Saskatchewan
・ Theodorescu
・ Theodoret
・ Theodoret of Antioch
・ Theodoriana
・ Theodorias
・ Theodorias (province)
・ Theodoric
・ Theodoric Borgognoni
・ Theodoric I
・ Theodoric I of Isenburg-Kempenich
・ Theodoric I of Paderborn


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Theodore, Australian Capital Territory : ウィキペディア英語版
Theodore, Australian Capital Territory

Theodore is a suburb in the Canberra, Australia district of Tuggeranong. The postcode is 2905. The suburb is named after Edward Glanville Theodore (1884–1950), a Queensland premier and deputy Prime Minister. It was gazetted on 5 August 1975.〔 Streets are named after people involved with the civilian war effort during the world wars.〔 The main street through the suburb is named after Sir Lawrence Wackett KBE, DFC, AFC, who is widely regarded as the "father of the Australian aircraft industry".
On Census night 2011, Theodore had a population of 4,020 people., and had a median age of 31 compared to the Australian median age of 37.
It is next to the suburbs of Conder and Calwell. It is bounded by the Monaro Highway and Tharwa drive. Located in the suburb is Theodore Primary School and a neighbourhood oval. It borders on Tuggeranong Hill and the Canberra Nature Park of Tuggeranong Hill nature reserve.
==Geology==

Deakin Volcanics of various kinds underlie the suburb. These are from the late Silurian age 414 Mya. Deakin Volcanics Rhyodacite and sediments are in the east. Deakin Volcanics red-purple and green grey rhyodacite are in the center. Deakin Volcanics green grey and purple rhyodacite are in the west. Deakin Volcanics cream rhyolite is in high south east parts. Quaternary alluvium is in the north lower parts, washed off the surrounding slopes.〔Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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