Gordon ACT 2906, 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 | 22 Oct 2020 | $795,000 | $785 |
| Sale | 12 Jan 2011 | $520,000 | $513 |
| Sale | 25 Nov 2004 | $365,000 | $360 |
| Sale | 12 Feb 2002 | $270,000 | $266 |
| Sale | 25 Nov 1991 | $68,000 | $67 |
Price per m² based on land size of 1012 m².
The property is a standalone house offering a private dwelling on its own lot
It features four bedrooms and two bathrooms, providing ample space for a family
The house sits on a 1,012 m² block, giving room for outdoor activities and potential landscaping
Gordon is about 0.8 km away, with Conder and Bonython roughly 1.4‑1.9 km away, and Calwell nearby as well
Point Hut Pond and its district park lie within the suburb, while Gordonvale Park and Pine Island Reserve are both within 2‑3 km of the home
The southern and central parts of Gordon contain Quaternary alluvium, whereas the northern section sits on Silurian‑age Deakin Volcanics rhyodacitic crystal tuff
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