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.
5 Cockle Street is a stand‑alone house. It is listed simply as a "House" in the property features
O'Connor is known for its leafy, heritage‑filled streets and predominantly detached single‑dwelling houses. The suburb also includes historic cul‑de‑sacs with heritage‑listed Tocumwal houses and a range of natural reserves
Yes, the heritage‑listed Tocumwal houses are located about 0.5 km away, and the Scout Hall, another heritage site, is also nearby within the suburb
The property is near the Bruce/O'Connor Ridge nature reserve, offering bush‑walking and mountain‑biking trails. Local sporting ovals for soccer, rugby and cricket are also within the O'Connor district
The O'Connor small shopping centre, which includes a bar, grocery store, several restaurants and a pharmacy, is situated within roughly 1 km of the house. This makes everyday amenities easily reachable on foot or by a short drive
The ground is formed mainly of calcareous shales from the Canberra Formation, overlain by Quaternary alluvium. In the western higher parts, Black Mountain Sandstone appears, while the northern ridge area contains Ordovician Greywacke from the Pittman Formation
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