Tharwa, Australian Capital Territory

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Tharwa Bridge and the Murrumbidgee River, 2005 (looking South); Tharwa is to the right. Despite recent rain, the flow was very low due to drought.

Construction of Tharwa Bridge 1893. Note the size of river before Tantangara Dam (1962) commenced diverting almost 50% of the river's flow.

Tharwa (postcode 2620) is a small village within the Australian Capital Territory, 35 kilometres south of Canberra, the capital city of Australia.

The village is located on the banks of the Murrumbidgee River and at the junction of Tidbinbilla and Naas Roads, and Tharwa Drive. The main public buildings are a general store, a preschool and primary school (now closed), Saint Edmund's Church, a cemetery, a community hall and tennis courts. The annual Tharwa Fair was hosted by the school, and was held in May until 2006.

1 History
2 Geology
3 See also
4 External links
- 4.1 Tharwa
- 4.2 External links

[edit] History

Tharwa is the oldest official settlement in the Australian Capital Territory, proclaimed a settlement in 1862. Tharwa was named after the Aboriginal word for Mount Tennent, the overlooking mountain which is part of Namadgi National Park. Mount Tennent was named after John Tennant, who was one the earliest and best-known bushrangers in the region. John Tennant lived in a hideout on the mountain behind Tharwa from which he raided local homesteads 1827-1828, before being arrested and transported to Norfolk Island.

Tharwa Bridge, opened on 27 March 1895, crosses the Murrumbidgee River. Tharwa Primary School was opened soon after, in 1899. The Tharwa township narrowly avoided being burnt in the 2003 Canberra bushfires. The Tharwa community is currently facing two further challenges: closures and repairs to Tharwa Bridge due to extensive rot in its supporting timbers discovered in 2005 and the 2006-07 Australian Capital Territory budget announcement of its plans to close the Tharwa preschool and primary school at the end of 2006.

[edit] Geology

Tharwa is in a different geological structural unit than the rest of Canberra, being on the Cotter Horst. The village itself is built on Tharwa Adamellite. This adamellite is coarsely foliated and contains biotite mica. It has been dated at 423 ±6 million years old. This places it in the upper Silurian age.

The outcrop area is extended to the north north west to Freshford, and includes Castle Hill. It goes as far to the west as Sawyer's Gully. To the south it goes close to Angle Crossing, and on the east side is bounded by the Murrumbidgee Fault. The Tharwa Adamellite is part of the Murrumbidgee Batholith.

The latitude and longitude of Tharwa is 35°31'00S 149°04'00E. The geoid is 19.356 meters above the theoretical ellipsoid shape of the earth at Tharwa. The astronomical measurement of the position on the earth's surface is only very slightly distorted by a non vertical gravitational field 0.3" to north and 0.6" to the west.

Magnetic declination at Tharwa is 11.817 deg east, total field strength is 43108 nT and magnetic inclination is -66.031 degrees; as at 1 March 2006.

Declination is increasing by 0.004 degrees per year. Inclination is increasing by 0.016 degrees per year (as in the rest of Canberra).

See also: Geology of the Australian Capital Territory