28 Waratah Street
28 Waratah Street, O'connor ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Sep 2014 | $153,600 | $231 |
Price per m² based on land size of 663 m².
Key details
- Locality
- O'connor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714889722
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/72/18
- Remoteness area
- Metro
- Property type
- House
- Land size
- 663 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 size of the land that the house at 28 Waratah Street sits on?
The property occupies a 663 m² block, providing ample space typical of O'Connor’s residential lots.
What type of dwelling can be found at 28 Waratah Street?
It is a detached single‑dwelling house, reflecting the suburb’s character of leafy, stand‑alone homes.
Which local shops and services are within easy walking distance of the house?
A small shopping centre in O'Connor offers a pub/bar, grocery store, a few restaurants and a pharmacy, all just a few minutes’ walk away.
How close are cafés and parks to the property?
Tilley's café in Lylyham is about 0.3 km away, and Jandura Park is roughly 0.5 km from the house, both within comfortable walking distance.
What public transport options are nearby?
The Dickson Interchange and the Macarthur Avenue light‑rail station are each approximately 0.9 km from the property, providing convenient metro access.
Are there any heritage or nature attractions close to 28 Waratah Street?
The suburb features heritage‑listed streets, the historic Tocumwal houses and Scout Hall, and the Bruce/O'Connor ridge nature reserve, a popular area for bushwalking and mountain biking.
What is the geological makeup of the O'Connor area?
The land is underlain by calcareous shales of the Canberra Formation overlain by Quaternary alluvium, with sections of Black Mountain Sandstone to the south and Greywacke of the Ordovician Pittman Formation to the north.