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 | 27 Jul 2013 | $570,000 | $828 |
| Sale | 16 Oct 1992 | $45,500 | $66 |
Price per m² based on land size of 688 m².
The home features four bedrooms and two bathrooms. Both are arranged within a single‑storey house layout
The residence stands on a 688 m² block. This provides ample outdoor space for gardening or recreation
The property includes two dedicated parking spaces. These are separate from any street parking and are part of the listed features
The house is located on the west side of Tharwa Drive in Gordon, ACT. It lies roughly 0.5 km from the centre of the Gordon suburb
Gordonvale Park is about 1.6 km away, and Beau and Jessi Park is approximately 2‑3 km distant. The suburb also contains the Point Hut Pond and district park within Gordon
The south and centre of Gordon are covered by Quaternary alluvium, while the northern part rests on Deakin Volcanics rhyodacitic crystal tuff from the Silurian age
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