30 Clianthus Street
30 Clianthus Street, O'connor ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Nov 2025 | Unknown | — |
Key details
- Locality
- O'connor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714899304
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/10/54
- Remoteness area
- Metro
- Property type
- House
- Internal area
- 121 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
How many bedrooms and bathrooms are in the house at 30 Clianthus Street?
The home features three bedrooms and one bathroom.
What parking options are available for this property?
The listing includes two parking spaces for residents.
What shopping and dining options are within walking distance of the property?
A small local shopping centre in O'Connor offers a pub/bar, a grocery store, a few restaurants, a pharmacy and other services, all within easy reach.
Which parks or sporting facilities are close to 30 Clianthus Street?
The property is near the O'Connor Ridge nature reserve, Jandura Park (about 1 km away), and the O'Connor district playing fields where soccer, rugby and cricket are commonly played.
Are there any heritage‑listed sites near the home?
Yes, the nearby Tocumwal houses are heritage‑listed, and the Scout Hall at Hovea Street and Boronia Drive is also on the ACT Heritage Council list, along with several Aboriginal sites on the Bruce and O’Connor Ridges.
How would you describe the overall character of O'Connor?
O'Connor is an affluent suburb noted for its leafy, heritage‑lined streets and predominantly detached single‑dwellings, giving it a pleasant, residential atmosphere.
What is the underlying geology of the O'Connor area?
The suburb sits on calcareous shales from the Canberra Formation overlain by Quaternary alluvium; the western higher parts consist of Black Mountain Sandstone, while the north, including O'Connor Ridge, contains Ordovician Greywacke of the Pittman Formation.