4 Karri Street
4 Karri Street, O'connor ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Apr 2025 | $1,147,500 | — |
Key details
- Locality
- O'connor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714900800
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/74/2
- Remoteness area
- Metro
- Property type
- Duplex-Semi-Detached
- Internal area
- 99 m²
- 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 dwelling is located at 4 Karri Street?
The property is a duplex‑semi‑detached home. It forms part of the leafy, heritage‑listed streets of O'Connor.
How many bedrooms and bathrooms does the home have?
The residence offers three bedrooms and one bathroom, providing comfortable accommodation for a small family or couple.
What parking is provided with the property?
The home includes one allocated parking space for residents.
What shopping and dining options are within easy reach of 4 Karri Street?
O'Connor features a small shopping centre with a pub/bar, a grocery store, a few restaurants and a pharmacy. A popular café, Tilley's, is just 0.4 km away, and a Vietnamese restaurant is located within the local shops.
Which parks or outdoor recreation areas are close to the property?
Jandura Park is about 0.4 km away, offering green space for recreation. The O'Connor Ridge nature reserve provides bushwalking and mountain‑biking trails, and the district playing fields host soccer, rugby and cricket matches.
Are there any heritage‑listed sites nearby?
Yes, O'Connor is known for its heritage‑listed streets, the Tocumwal houses (relocated post‑World War II) and the Scout Hall at the corner of Hovea Street and Boronia Drive.
What is the underlying geology of the O'Connor area?
The suburb sits on calcareous shales from the Canberra Formation, overlain by Quaternary alluvium. In the north, Greywacke from the Ordovician Pittman Formation is present, while the southern higher parts contain Black Mountain Sandstone.