27 Pedrail Place
27 Pedrail Place, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2021 | $680,000 | $1,312 |
| Sold | Aug 2016 | $485,000 | $936 |
| Sold | Feb 2009 | $380,500 | $734 |
| Sold | Aug 2001 | $57,800 | $111 |
| Sold | Jun 2001 | $179,500 | $346 |
Price per m² based on land size of 518 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847678
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/99/5
- Remoteness area
- Metro
- Property type
- House
- Land size
- 518 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
How many bedrooms and bathrooms does 27 Pedrail Place have?
The house offers three bedrooms and two bathrooms, providing ample space for a family or shared living.
What is the size of the land the property sits on?
The home is sited on a 518 m² block, giving room for a garden, outdoor entertaining or extra storage.
How many parking spaces are available at the property?
There are two designated parking spaces for residents, suitable for two vehicles.
What natural reserves or parks are nearby?
Dunlop Grasslands Nature Reserve and the nearby West Belconnen, Jarramlee and Fassifern Ponds are within the suburb, offering walking and wildlife‑watching opportunities.
How far is the property from the centre of the Dunlop suburb?
27 Pedrail Place is located about 0.4 km from the heart of Dunlop, making local shops and services easily reachable.
Which neighbouring suburbs are closest to the property?
The home borders the suburbs of Fraser, Charnwood and Macgregor, all just a short drive or walk away.
What geological features characterize the Dunlop area?
The suburb sits on Silurian‑age rocks, primarily Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west and the Deakin Fault running along its north‑east edge.