10 Polilight Street
10 Polilight Street, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jun 2015 | $255,000 | $439 |
| Sold | Apr 2004 | $361,000 | $622 |
| Sold | Jan 2003 | $98,000 | $168 |
Price per m² based on land size of 580 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847448
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/152/6
- Remoteness area
- Metro
- Property type
- House
- Land size
- 580 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 10 Polilight Street and how much land does it sit on?
It is a house situated on a 580 m² block of land.
How close is the property to the natural reserves and ponds that are part of the Ginninderra Catchment?
Dunlop contains the Dunlop Grasslands Nature Reserve as well as West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all of which are within the suburb and therefore a short walk from the home.
What parks or recreational areas are located nearby?
The Boslem And Harte Park is about 1‑2 km away, George Simpson Park is roughly 2‑3 km distant, and Goodwin Hill, a popular walking spot, lies around 2 km to the north‑east.
Which electoral districts does the suburb of Dunlop belong to?
For federal elections Dunlop is in the Division of Fenner, and for ACT Legislative Assembly elections it falls within the Ginninderra electorate.
What is the origin of the street name "Polilight Street"?
Polilight refers to a portable, high‑intensity filtered light source used by forensic scientists to detect fingerprints and other evidence.
What are the predominant geological features of the Dunlop area?
The suburb sits on Silurian‑age rocks, mainly 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 along the Deakin Fault.