68 Dryandra Street
68 Dryandra Street, O'connor ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jul 2009 | $755,000 | $748 |
Price per m² based on land size of 1009 m².
Key details
- Locality
- O'connor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714892038
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/84/33
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1009 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 are the key features of the house at 68 Dryandra Street?
The property is a detached house with three bedrooms and one bathroom, positioned on a 1,009 m² block of land.
How would you describe the character of the O'Connor suburb where the property is located?
O'Connor is known for its leafy, heritage‑listed streets and predominantly detached single‑dwelling houses, giving the area a quiet, suburban feel with plenty of mature trees.
Are there any heritage‑listed sites near 68 Dryandra Street?
Yes, the Tocumwal houses, heritage‑listed ex‑government homes, are located about 0.4 km away, and the suburb also includes other heritage listings such as the Scout Hall.
What natural or recreational areas are close to the property?
The Bruce/O'Connor ridge nature reserve and the O'Connor Ridge bush‑walking and mountain‑biking tracks lie within the suburb, and Jandura Park is just around 1.3 km away.
What local amenities can residents access nearby?
A small shopping centre in O'Connor offers a pub/bar, grocery store, several restaurants and a pharmacy, while Alivio Tourist Park (0.8 km) and Canberra Olympic FC (0.9 km) are also within walking distance.
What geological features characterize the area around 68 Dryandra Street?
The land is underlain by calcareous shales of the Canberra Formation overlain by Quaternary alluvium, with nearby sections of Black Mountain Sandstone and Greywacke from the Ordovician Pittman Formation.