3 Finn Street
3 Finn 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.
- GAACT714910956
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/56/7
- Remoteness area
- Metro
- Property type
- House
- Land size
- 780 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 parcel for 3 Finn Street?
The property sits on a 780 m² block. This provides ample space for garden or outdoor activities typical of the suburb’s spacious lots.
How many bedrooms does the house at 3 Finn Street have?
The home features four bedrooms. It offers generous family accommodation within a single‑storey layout.
What type of dwelling is located at 3 Finn Street?
It is a detached house, reflecting O'Connor’s characteristic leafy streets and single‑dwelling homes. The design fits the suburb’s heritage‑rich residential character.
Are there any heritage or natural sites near the property?
Yes, the heritage‑listed Tocumwal houses are only about 0.2 km away, and the Bruce/O'Connor ridge nature reserve lies nearby. The O'Connor Ridge provides bush‑walking and mountain‑biking trails within the area.
What shopping and dining options are close to 3 Finn Street?
A small local shopping centre offering a pub/bar, grocery store, a couple of restaurants and a pharmacy is located within roughly 1 km of the home. These amenities serve everyday needs conveniently.
What recreational facilities are available in the O'Connor district?
The O'Connor district playing fields host soccer, rugby and cricket matches, and nearby parks such as Gazetted Park and Jandura Park provide green space for leisure. These facilities are all within easy walking distance.
What is the geological composition of the land in O'Connor?
The area sits on calcareous shales from the Canberra Formation, overlain by Quaternary alluvium. Higher western parts feature Black Mountain Sandstone, while the northern ridge includes Ordovician Greywacke.