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
- 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 type of property is located at 18 Polwarth Circuit?
It is a freestanding house situated on a 485 m² block of land. The property is part of the Dunlop suburb in Canberra.
How close is the house to the Dunlop Grasslands Nature Reserve?
The Dunlop Grasslands Nature Reserve lies at the edge of the suburb, making it adjacent to the property. Residents can easily access the reserve for walking and wildlife observation.
What nearby natural attractions can residents enjoy?
Within a short distance are West Belconnen Ponds, Jarramlee Pond, and Fassifern Pond, all part of the Ginninderra Catchment. These water bodies and surrounding parks provide recreational walking and cycling trails.
How far is the property from the neighbouring suburb of Charnwood?
Charnwood is approximately 1.6 km away, reachable by local roads within a few minutes by car.
What is the distance to Goodwin Hill from 18 Polwarth Circuit?
Goodwin Hill is about 1.6 km north‑west of the property, offering scenic views and walking opportunities.
Which electoral districts cover this address?
For Australian federal elections the location falls in the Division of Fenner. In ACT Legislative Assembly elections it is part of the Ginninderra electorate.
What are the main geological features of the Dunlop area?
The suburb sits on Silurian‑age rocks, dominated by Deakin Volcanics purple rhyodacite. Grey tuff from the Laidlaw Volcanics overlays the south‑west, and the Deakin Fault runs along the north‑east edge, exposing green‑grey dacite and quartz‑andesite of the Hawkins Volcanics.