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  2. Daniel Murphy

    https://www.utas.edu.au/library/companion_to_tasmanian_history/M/Daniel%20Murphy.htm
    25 Jun 2012: Daniel Murphy. Cardinal Moran, Archbishop Murphy and other clergy, 1880s (ALMFA, SLT). Daniel Murphy (1815–1907), second Catholic Bishop and first Archbishop of Hobart, was ordained in Ireland in 1838, and worked in India until his transfer to

  3. Battery Point

    https://www.utas.edu.au/library/companion_to_tasmanian_history/B/Battery%20Point.htm
    25 Jun 2012: Battery Point. Battery Point is the background for this 1878 photo of Hobart's docks: the 'new wharf', warehouses, signal station, and, top right, dwellings (W. L. Crowther library, SLT). Battery Point is that landform along the southern shore of

  4. Campbell Town

    https://www.utas.edu.au/library/companion_to_tasmanian_history/C/Campbell%20Town.htm
    25 Jun 2012: CAMPBELL TOWN. The main street of Campbell Town in the 1920s (Tasmaniana Library, SLT). Campbell Town was named by Governor Lachlan Macquarie in 1821 after his wife's family. 1. There was already some European settlement in the area. Native

  5. Mount Strzelecki

    https://www.utas.edu.au/library/companion_to_tasmanian_history/M/Mt%20Strzelecki.htm
    25 Jun 2012: Mount Strzelecki. Bishop Nixon's sketch of the peaks of Flinders Island, 1857 (ALMFA, SLT). Mount Strzelecki at 756 metres is the highest peak of the Furneaux Group of islands. Set in the Strzelecki National Park in the south of Flinders Island, it

  6. Mount Wellington

    https://www.utas.edu.au/library/companion_to_tasmanian_history/M/Mt%20Wellington.htm
    25 Jun 2012: Mount Wellington. Mary Morton Allport, 'Sun-rise on Mt. Wellington', undated (ALMFA, SLT). Mount Wellington lies directly behind Hobart and is the city's dominant feature. It is 1,270 metres high and was formed during the Permian, Triassic and

  7. River Derwent

    https://www.utas.edu.au/library/companion_to_tasmanian_history/R/River%20Derwent.htm
    25 Jun 2012: River Derwent. HS Melville, 'On the Derwent, Hobarton', no date, perhaps 1830s? (W. L. Crowther Library, SLT). The River Derwent flows from Lake St Clair in Tasmania's Central Plateau and, after a course of 182 kilometres, discharges into Storm Bay.

  8. Paint Pigment

    https://www.utas.edu.au/library/companion_to_tasmanian_history/P/Paint%20pigment.htm
    25 Jun 2012: Paint Pigment. Small deposits of weathered ochre are common across Tasmania, resulting from the weathering of a variety of sources, such as dolerite, basalt, haematite and serpentinite. The use of both red and yellow ochre mixed with animal fat as a

  9. Anglo-Indians

    https://www.utas.edu.au/library/companion_to_tasmanian_history/A/Anglo-Indians.htm
    25 Jun 2012: Anglo-Indians. Edward Braddon, the best-known of the Anglo-Indian immigrants (AOT, PH30/1/296C). In Tasmania the term 'Anglo-Indians' appears to cover English people who resided in India (at the time part of the British Empire) then in Tasmania,

  10. Northern Club

    https://www.utas.edu.au/library/companion_to_tasmanian_history/N/Northern%20Club.htm
    25 Jun 2012: Northern Club. The Northern Club, modelled on the English gentlemen's club, was established in Launceston in 1894 with sixteen members, each subscribing two guineas. Membership increased to 150 within three years, necessitating a move to larger

  11. Popular Music

    https://www.utas.edu.au/library/companion_to_tasmanian_history/P/Popular%20music.htm
    25 Jun 2012: Popular Music. Findlays Acrobatic and Ragtime Band, about 1910 (AOT, PH30/1/4385). Popular music developed in the nineteenth century, mainly as music at local dances. By the 1920s, dances were a major form of entertainment. Music ranged from locals
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