Conder ACT 2906, Australia
Key points for 14 Handasyde Street.
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 | 12 Sep 2003 | $440,000 | $535 |
| Sale | 26 Sep 1997 | $248,500 | $302 |
| Sale | 5 Jun 1995 | $245,000 | $298 |
| Sale | 30 Jul 1993 | $53,900 | $65 |
Price per m² based on land size of 822 m².
The property offers 4 bedrooms and 2 bathrooms, providing ample space for a family
The house is positioned on an 822 m² block, offering a sizable yard for outdoor activities
Within a short walk you’ll find Gordonvale Park (about 1.2 km away) and Beau and Jessi Park (around 1.3 km), both popular for walking and picnics
It is roughly 0.3 km from the suburb centre of Conder, which includes Lanyon Market Place and local shops
Tuggeranong Hill is situated approximately 1 km to the south, offering scenic views and walking tracks
The suburb is covered by Quaternary alluvium, while the surrounding hills consist of Silurian‑age Deakin Volcanics, including ignimbrite and tuff
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