O'connor ACT 2602, Australia
Based on curated rent estimate.
Confidence ratings show how closely the estimate matches the comparable property data we currently have.
There is a stronger pool of recent, relevant comparison data and the subject property lines up closely with those comparable properties.
There is a reasonable amount of comparison data, but the closest matches may vary more in type, size, timing or location.
There are fewer recent comparable properties available, or the known examples are less similar to the subject property.
These figures are estimates and broad indications only. They are generated from recorded property attributes and available third-party market data, without a physical inspection of the property.
They are not a professional valuation, appraisal, legal opinion or financial recommendation. No person should rely on them as the sole basis for a purchase, sale, lease, lending or investment decision.
Yardize does not guarantee the accuracy or completeness of any rent estimate, value estimate, range or confidence score, and no legal claim can be made against us for reliance on this information.
Based on the comparable property evidence currently available.
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sale | 21 Oct 2009 | $550,000 | $618 |
| Sale | 14 Jan 2002 | $305,000 | $343 |
Price per m² based on land size of 889 m².
The property sits on a block of about 889 m²
It provides four bedrooms
It is a detached single‑dwelling house typical of O'Connor’s leafy streets
O'Connor features heritage‑listed streets, the Bruce/O'Connor ridge nature reserve, the historic Tocumwal houses, and the listed Scout Hall, alongside Aboriginal heritage sites on the ridges
A small shopping centre with a pub/bar, grocery store, several restaurants and a pharmacy is nearby, as well as the O'Connor Uniting Church and the Canberra Olympic FC football club within about a kilometre
The house is roughly 0.8 km from the centre of the O'Connor suburb
The suburb sits on calcareous shales of the Canberra Formation overlain by Quaternary alluvium, with higher western parts comprising Black Mountain Sandstone and Greywacke from the Ordovician Pittman Formation
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