1821 Info 1c3: Caleb Crompton |
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On the afternoon of 09 November 2015, I found Trafalgar and its 1817 farmhouse
- reputed to be the oldest standing in Australia on its original foundation of
Tertiary basalt rock foot print. The present owner, Trevor Couchman, was there trying
to renovate, under the unfunded guidance of Heritage Tasmania, the heavily neglected
interior and the dilapidated out buildings. The previous owner, a member of the Hart
family, had moved out in 2013, aged 92, after living there since a girl.
When Heather Schoffelen visited in November 2017, the project was still recognisable. This is to be a lengthy project. Work in hand. Trafalgar is listed on the Tasmania Heritage Register and is afforded statutory
protection under the Historic Cultural Heritage Act 1995.
‘A
person must not carry out any works in relation to a registered
place...which may affect the historic cultural heritage significance of the place
unless
the works are approved by the Tasmanian Heritage
Council.’ |
The agricultural land is brown clay soils developed on tertiary basalts to form gently rolling to undulating land. Lower land, towards Rose Rivulet, is deeply dissected tertiary sediments.
The area has a cool, wet climate typical of inland northern Tasmania. The closest climatic data source to the study area is that taken by the Bureau of Meteorology (BOM) is at Launceston Airport. The data shows that rainfall occurs throughout the year; with a mean annual rainfall of 589mm. Rainfall is highest in August and September (64 –71mm) and lower from January to February (28 –31mm). The warmest months of the year are January and February, when mean temperatures range from minimums of 10°C to maximums of about 23°C. Winter tends to be cold with mean annual temperatures in the coldest months of June and July ranging from 1.5°C mean minimum to maximum temperatures of about 11°C (BOM 2015).
The largest water courses crossed by these corridor branches are the Rose Rivulet, Springvale Creek and Briarly Creek. Rose Rivulet is a semi-permanent water course that has its’ headwaters in the hills just to the south-east of the Dalness Dam site. The rivulet flows in a north-west direction, eventually rejoining with the North Esk River, near Relbia, on the outskirts of Launceston. Springvale Creek also a semi-permanent water course that has its’ headwaters in the Devon Hills to the south-west of the site. The creek flows in a north-east direction, eventually joining with the Rose Rivulet approximately 2km to the north-east of the site.
Springvale Creek site of isolated and scattered aboriginal artefact
Aerial views of Trafalgar and Spring Vale
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Above: Aerial view locating Spring Vale 2016 |
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Above: Aerial view locating Trafalgar 2014 |
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Above: Aerial view locating Trafalgar and Spring Vale 2016 |
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Above: Aerial view of Talisker 2016 |
Photo locations of Barclay land in 2015
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Above: Map locating modern Springvale Creek, running south- west to north-east and showing location and directions of photos above |
Hoverbox Photo Gallery - Springvale Creek and Trafalgar land,
Author: November
2015 This feature does not function correctly on phones and tablets The numbered images relate to the following map |
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1. Springvale Creek head waters at Western Junction 2. Springvale Creek enters Rose Rivulet |
3. McLeod land looking towards Launceston Airport |
1 | 2 | 3 |
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4. Trafalgar land from Trafalgar Lane | 5. Barclay land across the South Esk | 6. Trafalgar land looking east |
4 | 5 | 6 |
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Scenes of Trafalgar in 2015
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This page was created by Richard Crompton and maintained by Chris Glass |
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Version A9 Updated 07 June 2023 |