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 | 1 Feb 2022 | $950,000 | $1,399 |
| Sale | 21 Mar 2011 | $353,000 | $519 |
| Sale | 16 May 2002 | $314,000 | $462 |
| Sale | 7 Sep 1995 | $180,000 | $265 |
| Sale | 12 Apr 1994 | $60,000 | $88 |
Price per m² based on land size of 679 m².
It is a detached house offering four bedrooms and two bathrooms
The house sits on a 679 m² block, providing ample outdoor space
The property includes two parking spaces
Gordonvale Park is about 1.4 km away, Beau and Jessi Park is roughly 1.7 km away, and the broader Lanyon Valley is within 0.7 km
Tuggeranong Hill is approximately 0.7 km to the north, offering easy access to walking tracks
Conder is part of Canberra’s southernmost suburbs in the Lanyon Valley, known for rapid population growth and strong year‑on‑year house price appreciation
The area is covered by Quaternary Alluvium, with underlying Silurian‑age Deakin Volcanics such as ignimbrite and tuff on the surrounding hills
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