Banks 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 | 26 Jun 2011 | $529,000 | $729 |
| Sale | 13 May 2003 | $339,000 | $467 |
| Sale | 6 Jul 1994 | $57,500 | $79 |
| Sale | 17 Jun 1993 | $50,000 | $68 |
Price per m² based on land size of 725 m².
The home features four bedrooms and two bathrooms, providing ample space for families or guests
It sits on a 725 m² block, offering a generous yard for outdoor activities or future development
It is a standalone house, a detached residence typical of the Banks suburb
Beau and Jessi Park is about 0.5 km away, and Gordonvale Park is roughly 1.4 km distant, both offering green space for walks and play
To the east lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the smaller Big Monks mountain with a gliding stage is also accessible nearby
The surface of Banks is covered by alluvium, while the surrounding hills are formed from Deakin Volcanics that erupted in the Silurian age about 414 million years ago
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