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 | 3 Feb 2007 | $500,000 | $482 |
| Sale | 7 Jan 1999 | $227,000 | $219 |
| Sale | 28 Nov 1990 | $41,000 | $39 |
Price per m² based on land size of 1036 m².
It is a standalone house situated on a 1,036 m² block in the suburb of Gordon, ACT
The land size is 1,036 m², providing ample space for gardens, outdoor activities, or future extensions
Barneys Hill, a local mountain, is about 0.6 km away, Pine Island Reserve is roughly 1.5 km away, and both Stranger Pond and Isabella Pond lie within 2 km, offering easy access to nature
The house is approximately 1.1 km from the centre of the Gordon suburb
Gordon is bordered by the suburbs of Bonython, Conder, and Banks, all located within about 1–2 km
The southern and central parts of Gordon rest on Quaternary alluvium, while the northern section is covered by Silurian‑age Deakin Volcanics rhyodacitic crystal tuff
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