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Murrumbateman is a town in the Southern Tablelands of New South Wales, Australia. It is on the Barton Highway , approximately 30 kilometres north-west of Canberra , and is part of the Yass Valley Shire .
The Canberra District wine region is located around Canberra in the Capital city of Australia.It covers the northern part of the Australian Capital Territory and an area of New South Wales to the east and north of that, including towns of Bungendore, Murrumbateman and Yass, New South Wales.
The Canberra wine region is a cool climate area and the wines produced by Clonakilla reflect this. Around 10,000 to 12,000 cases of wine are produced each year. [13]The flagship wine is the Shiraz Viognier co-fermentation, produced from a selection of the best grapes in a single twelve hectare vineyard.
Barton Highway commences at the interchange with Hume Highway northeast of Yass and heads in a southerly direction as a four-lane, dual-carriageway freeway, before narrowing to a two-lane, single-carriageway highway south of the interchange with Yass Valley Way where it meets its old alignment, and continues south through undulating hills to the village of Murrumbateman, before crossing the ...
Europeans first settled Canberra and surrounding region during the 1830s which was known as Ginninderra. A road between Murrumbateman and Bungendore passed through nearby Mulligans Flat. A row of mature trees mark the alignment of the coach route to Bungendore.
Gunning is a small town on the Old Hume Highway, between Goulburn and Yass in the Southern Tablelands of New South Wales, Australia, about 260 km south-west of Sydney and 75 km north of the national capital, Canberra. Nearby towns and cities are Cullerin, Gundaroo, Dalton, Yass, Murrumbateman and Goulburn.
The third Ginninderra smith was George Curran. Curran married Mary Ann Hatch, the niece of the original smith. George's younger brother, John Curran, became the blacksmith at Murrumbateman, which meant that the brothers dominated the blacksmithing trade between Murrumbateman and Ginninderra in the 1876-89 period. [11]
East of Canberra deep water of the Monaro Basin remained in the Captains Flat area. A second unconformity occurred after the Black Mountain Sandstone was uplifted and eroded at the end of the early Silurian. This was called the Quidongan Deformation. The Canberra formation was deposited in shallow water with limestone, and shale
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