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 | 4 Nov 1998 | $95,000 | $95 |
| Sale | 18 Aug 1997 | $98,000 | $98 |
Price per m² based on land size of 990 m².
The house offers four bedrooms and two bathrooms, providing ample space for families or guests
The property occupies a 990 m² block, giving room for outdoor activities and potential landscaping
It is a detached house with two dedicated parking spaces for residents and visitors
Gordon is on the west side of Tharwa Drive in the Tuggeranong district of Canberra. It is adjacent to the suburbs of Bonython, Conder and Banks
Gordonvale Park is about 1.6 km away, Beau and Jessi Park is roughly 2.4 km distant, and Pine Island Reserve is around 2.5 km from the property. The suburb also contains the Point Hut Pond and Point Hut district park
The southern and central parts of Gordon rest on Quaternary alluvium, while the northern section has surface exposures of Silurian‑age Deakin Volcanics rhyodacitic crystal tuff
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