26 Macpherson Street
26 Macpherson 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.
- GAACT714885450
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/61/11
- Remoteness area
- Metro
- Property type
- House
- Land size
- 774 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 on which 26 Macpherson Street sits?
The property sits on a 774 m² block, offering a generous garden area typical of detached houses in O'Connor.
What type of residence is located at 26 Macpherson Street?
It is a stand‑alone house, reflecting the suburb’s character of detached single‑dwelling homes on leafy streets.
How would you describe the heritage and natural setting of the O'Connor suburb?
O'Connor is known for its leafy, heritage‑listed streets, historic Tocumwal houses, and the nearby Bruce/O'Connor ridge nature reserve that provides bush walking and mountain‑biking trails.
What shopping and dining amenities are close to the property?
A small local shopping centre a short walk away includes a pub/bar, a grocery store, several restaurants, a pharmacy and a bicycle shop.
Which recreational facilities are within walking distance of 26 Macpherson Street?
Canberra Olympic FC is about 0.2 km away, and parks such as Jandura Park (≈0.7 km) and Gazetted Park (≈0.8 km) provide open spaces for sport and leisure.
How near are public transport options like light rail stations to the home?
The Macarthur Avenue light rail station and the Ipima Street Metro station are each about 1 km from the property, offering convenient access to Canberra’s public transport network.
What geological features underlie the area around 26 Macpherson Street?
The site sits on calcareous shales from the Canberra Formation, overlain by Quaternary alluvium, with nearby higher ground composed of Black Mountain Sandstone and Greywacke from the Ordovician Pittman Formation.