61 Wattle Street
61 Wattle Street, O'connor ACT 2602, Australia
Key details
- Locality
- O'connor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714907052
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/75/17
- 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 kind of residence is 61 Wattle Street?
It is a detached four‑bedroom house situated on a 663 m² block. The property offers ample land for a family home in O'Connor.
How is the suburb of O'Connor characterised?
O'Connor is an affluent, leafy suburb known for its heritage‑listed streets and mature trees. It features detached homes, historic cul‑de‑sacs and a strong sense of community.
Which parks or outdoor spaces are close to the home?
Jandura Park is about 0.3 km away, providing walking and play areas. The O'Connor Ridge nature reserve and district playing fields also offer bushwalking, mountain biking and sports nearby.
What public transport options are within walking distance?
The Macarthur Avenue light‑rail station is roughly 0.7 km away, and the Dickson Interchange is about 0.8 km from the property, giving easy access to Canberra’s Metro network.
What shopping and dining amenities can be found nearby?
The O'Connor small shopping centre hosts a bar, grocery, pharmacy and several restaurants. A café, Tilley’s, is just 0.5 km away, and additional dining options are available in nearby Lyneham.
Are there heritage‑listed sites in the neighbourhood?
Yes, O'Connor includes heritage‑listed streets, the Scout Hall on Hovea Street, and the Tocumwal Houses, historic homes moved from RAAF Station Tocumwal after World War II.
What geological features underlie the O'Connor area?
The suburb sits on calcareous shales of the Canberra Formation, overlain by Quaternary alluvium. Higher western parts contain Black Mountain Sandstone, while the ridge has Ordovician Greywacke.