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 | 27 Jul 1995 | $54,000 | $47 |
Price per m² based on land size of 1129 m².
The house features four bedrooms and three bathrooms, providing ample space for families or guests
The property sits on a 1,129 m² block, offering a generous yard for outdoor activities and landscaping
Tuggeranong Hill is about 1.1 km away and Callaghan Hill about 1.5 km away. Parks such as Beau and Jessi Park (≈1.8 km) and Gordonvale Park (≈2.2 km) are also nearby
An electrical substation is roughly 0.4 km from the house, and the former Theodore weather station on Conlon Street lies about 1.4 km away
Conder is a southern Canberra suburb in the Lanyon Valley, noted for its artistic street names, rapid population growth, and key services such as the Lanyon Market Place
The suburb sits on Quaternary alluvium, while the surrounding hills are composed of Silurian‑age Deakin Volcanics, including ignimbrite and tuff formations
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