31 Wongoola Close
31 Wongoola Close, O'connor ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2022 | $2,600,000 | — |
Key details
- Locality
- O'connor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714899330
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/32/74
- Remoteness area
- Metro
- Property type
- House
- 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 residence is located at 31 Wongoola Close?
It is a detached house offering four bedrooms and two bathrooms. The property also includes two designated parking spaces.
How many parking spaces are provided with the home?
The residence comes with two parking spaces, as listed in the property features.
What leisure and sporting facilities are nearby?
Within about 1–2 km you’ll find the Australian Institute of Sport, Canberra Stadium, and Jandura Park. The O'Connor district playing fields also host soccer, rugby, and cricket matches.
Which heritage attractions are close to the address?
The Tocumwal houses, heritage‑listed ex‑government homes, are just 0.6 km away. O'Connor’s leafy streets and several heritage‑listed sites add historic character to the area.
What shopping and dining options are available nearby?
A short walk (about 0.8 km) brings you to the O'Connor shopping centre, which includes a bar, a restaurant, a supermarket, a pharmacy and other small retailers.
What natural areas can be enjoyed from this location?
The suburb features the O'Connor Ridge, part of Canberra Nature Park, offering bushwalking and mountain‑biking trails. The nearby Bruce/O'Connor ridge nature reserve also provides extensive tree‑lined paths.
What is the underlying geology of the O'Connor area?
The ground consists of calcareous shales from the Canberra Formation overlain by Quaternary alluvium, with Black Mountain Sandstone in the western higher parts and Greywacke from the Ordovician Pittman Formation in the north.