50 Scrivener Street
50 Scrivener 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.
- GAACT714900791
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/74/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 589 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 dwelling is located at 50 Scrivener Street?
The property is a detached house set on a 589 m² block of land.
How would you describe the character of the O'Connor suburb where the house is located?
O'Connor is an affluent, leafy suburb of Canberra known for its heritage‑listed streets, detached single‑dwelling homes, and abundant trees on the Bruce/O'Connor ridge nature reserve.
What heritage or natural attractions are close to 50 Scrivener Street?
The home is within walking distance of the Bruce/O'Connor ridge nature reserve, the heritage‑listed Tocumwal houses, and the Scout Hall at Hovea Street, all part of the suburb’s historic landscape.
Which community amenities can be found nearby?
A short stroll (about 0.1 km) leads to O'Connor Uniting Church, and within 0.5 km there is the O'Connor shopping centre with a bar, restaurant, grocery store and pharmacy, as well as Tilley's café and Jandura Park.
What sports or recreation facilities are available close to the property?
The O'Connor district playing fields host soccer, rugby and cricket, and Jandura Park (≈0.5 km away) offers open green space for walking and informal sports.
How far is the nearest light‑rail station from the house?
The Macarthur Avenue light‑rail station is about 1 km away, providing easy access to Canberra’s Metro network.
What geological features underlie the land in O'Connor?
The area sits on calcareous shales from the Canberra Formation overlain by Quaternary alluvium, with sections of Black Mountain Sandstone in the higher western parts and Ordovician Greywacke on the O'Connor Ridge.