26 Branson Street
26 Branson Street, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2008 | $555,000,645,000 | $640,878,342 |
Price per m² based on land size of 866 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714874582
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/155/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 866 m²
- Internal area
- 269 m²
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Real Estate Agencies
Nearby schools
Frequently asked questions
What is the price range for 26 Branson Street?
The listed price range for the house is between $555,000 and $645,000.
How many bedrooms and bathrooms does the property have?
The home offers four bedrooms and three bathrooms.
What parking options are provided with the house?
The property includes two dedicated parking spaces.
How far is 26 Branson Street from Canberra's city centre?
It is situated about 11.6 km (approximately 7 mi) north‑west of Canberra’s central business district.
What natural reserves or parks are close to the property?
Nearby you’ll find the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond, Fassifern Pond, as well as Boslem And Harte Park (≈1.6 km) and George Simpson Park (≈2.4 km).
Which suburbs border Dunlop?
Dunlop is adjacent to the suburbs of Fraser, Charnwood and Macgregor, with Charnwood about 1.4 km away and Fraser roughly 1.9 km distant.
Who was the suburb of Dunlop named after?
The suburb is named in honour of Lieutenant Colonel Sir Ernest Edward “Weary” Dunlop, an Australian surgeon celebrated for his leadership as a POW during World War II.
What geological features are characteristic of the Dunlop area?
The area is underlain mainly by Silurian‑age Deakin Volcanics purple rhyodacite, with patches of grey tuff from the Laidlaw Volcanics and uplifted green‑grey dacite and quartz‑andesite of the Hawkins Volcanics near the north‑east Deakin Fault.