Conder 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 | 7 Apr 2011 | $440,000 | $526 |
| Sale | 28 Feb 2000 | $145,000 | $173 |
| Sale | 24 Jul 1991 | $41,500 | $49 |
Price per m² based on land size of 835 m².
It is a standalone house
The property sits on 835 m² of land, offering generous space for outdoor activities
The house is in Conder, a suburb in the Lanyon Valley of Canberra’s Tuggeranong district, known as one of the city’s southernmost suburbs
Conder hosts the Lanyon Market Place, a central retail hub, and one of Canberra’s four Vikings clubs, serving as key local services
Beau and Jessi Park is about 1.1 km away, while Gordonvale Park is roughly 1.3 km from the house, both within easy walking distance
Tuggeranong Hill, a prominent mountain, is located approximately 1.1 km to the north of the house
The area is covered by Quaternary Alluvium, and beneath it the surrounding hills consist of Silurian‑age Deakin Volcanics, including ignimbrite and tuff
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