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

Yarralumla is a large inner south suburb of Canberra, the capital city of Australia. Located approximately south-west of the city, Yarralumla extends along the south-west bank of Lake Burley Griffin. (The lake was created after the Second World War through the blocking, with a dam, of the Molonglo River.)
Europeans first settled the area in 1828, and it was named Yarralumla in 1834 from the indigenous Ngunnawal people's term for the area. (It is also spelt "Yarrowlumla" on some 19th-century maps and other documents.) Frederick Campbell, grandson of Robert Campbell who built nearby "Duntroon", completed the construction of a large, gabled, brick house on his property in 1891 that now serves as the site of Government House, the official residence of the Governor-General of Australia. Campbell's house replaced an elegant, Georgian-style homestead, the main portions of which were erected from local stone in the 1830s. Among the old Yarralumla homestead's most notable occupants were Sir Terence Aubrey Murray, who owned Yarralumla sheep station from 1837 to 1859, Augustus Onslow Manby Gibbes, who owned the property from 1859 to 1881, and Augustus' father Colonel John George Nathaniel Gibbes (1787–1873). (Augustus "Gussie" Gibbes was Murray's brother-in-law; he also advanced money to Frederick Campbell to assist with the construction, in 1890–1891, of Campbell's grand new family house at Yarralumla.)
The modern suburb of Yarralumla was gazetted by the government in 1928 and as of 2011 was home to approximately 3,000 people and many diplomatic missions. In recent years, it has become one of Canberra's most desirable and expensive residential suburbs because of its wide leafy streets, attractive lakeside setting and central location.
== Geography ==
Yarralumla is located in the central Canberra district of South Canberra. It is bordered by Lake Burley Griffin to the north, Commonwealth Avenue and Capital Hill to the east, Adelaide Avenue and the Cotter Road to the south, and Scrivener Dam, Lady Denman Drive and part of the Molonglo River to the west.〔''UBD Canberra'', pp. 58–59.〕
Although Yarralumla is one of the largest suburbs in Canberra by area,〔''UBD Canberra'', pp. 1–100.〕 its population remains quite small because more than half of its area consists of open space or non-residential development, including Weston and Stirling Parks, the Royal Canberra Golf Club, and the grounds of Government House.〔 A relatively high proportion of houses are occupied by diplomatic missions.〔
The embassy area of Yarralumla is located towards the eastern end of the suburb next to Stirling Park.〔 It is the hilliest area of Yarralumla; Parliament House and the Parliamentary Triangle are located nearby.〔
The streets in Yarralumla are named after Australian governors and botanists.〔(【引用サイトリンク】 Suburb Name search results )〕 Most of the older streets in the suburb are laid out on an approximately rectangular grid with some curved sections, while the more hilly eastern end of the suburb, including the embassy district, is set out with contour-guided roads.〔 Major roads in Yarralumla include Banks Street, Novar Street and Hopetoun Circuit in a north-south direction and Schlich Street, Loftus Street and Weston Street running east-west. Being a dormitory suburb, there are no major through roads.〔 Access to the rest of the city can be made from Adelaide Avenue, Commonwealth Avenue, Lady Denman Drive and Cotter Road, all of which run along the borders of the suburb.〔 From these roads, entry to the suburb can be gained by turning into roads such as Coronation Drive, Hopetoun Circuit and Novar Street.〔
Yarralumla is located on the Yarralumla Formation which is a mudstone/siltstone formation that was formed around 425 million years ago during the Silurian Period. The formation extends from Red Hill and Woden in the South to Lake Burley Griffin in to the north, passing under the suburb of Yarralumla. The formation is evidence of the last major marine sedimentary period when eastern Australia was still covered by shallow seas. It shows fossil evidence of trilobites, coral and primitive crinoids. The Yarralumla brickworks quarry and the Deakin anticline are places where the formation is exposed and easily studied.〔(【引用サイトリンク】 Yarralumla Brickworks Entry 2004 )

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