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 | 18 Dec 1991 | $108,000 | $203 |
| Sale | 1 May 1991 | $29,400 | $55 |
Price per m² based on land size of 531 m².
The property sits on a 531 m² block. This provides ample space for a garden or outdoor entertainment area
The address is on the west side of Tharwa Drive in the suburb of Gordon, ACT. Gordon is part of the Tuggeranong district of Canberra
Gordonvale Park is about 0.4 km away, and Beau and Jessi Park is approximately 1‑2 km distant. Both parks are within easy walking distance for recreation
Gordon borders the suburbs of Bonython, Conder and Banks. Conder is roughly 0.8 km from the property
Gordon is named after the poet Adam Lindsay Gordon (1833–1870). The suburb was officially gazetted on 12 March 1987
The southern and central parts of Gordon contain Quaternary alluvium, while the northern area has Deakin Volcanics rhyodacitic crystal tuff from the Silurian age
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