18 Polwarth Circuit
18 Polwarth Circuit, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Feb 2015 | $455,000 | $938 |
| Sold | Jun 2002 | $203,900 | $420 |
Price per m² based on land size of 485 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847551
- Commonwealth electorate
The federal electorate this address is in (for Australia's Parliament).
- Fenner
- State lower house
The state electorate this address is in (lower house).
- Ginninderra
- Remoteness area
- Metro
- Property type
- House
- Land size
- 485 m²
- Internal area
- -
- 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 land size of the property at 18 Polwarth Circuit?
The house sits on a 485 m² block. This provides a modest yard area within the Dunlop suburb.
How far is 18 Polwarth Circuit from the Canberra city centre?
Dunlop is located approximately 11‑12 km north‑west of Canberra’s centre, so the property is about that distance from the city.
What natural reserves or parks are nearby?
The property is close to several nature areas, including the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond. The Boslem And Harte Park is also roughly 1.5‑2 km away.
Which estates are part of the Dunlop suburb?
Dunlop contains several small estates: The Meadows, Ginninderra Ridge, Ginninderra Ponds, Dunlop Hills and Jarramlee Park. Each estate has its own distinctive signage.
What is the origin of the street name ‘Polilight Street’?
Polilight Street is named after the Polilight, a portable high‑intensity filtered light used by forensic scientists to detect fingerprints and other trace evidence.
What geological features are characteristic of Dunlop?
Dunlop sits on Silurian‑age rocks, primarily Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west. The Deakin Fault runs along the north‑east edge, and Hawkins Volcanics dacite and quartz‑andesite are uplifted north of the fault.