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 | 21 Nov 2019 | $470,000 | $1,208 |
| Sale | 24 Jul 2009 | $370,000 | $951 |
| Sale | 10 Jul 2008 | $340,000 | $874 |
| Sale | 31 Jan 2001 | $132,000 | $339 |
| Sale | 26 Oct 1992 | $27,500 | $70 |
Price per m² based on land size of 389 m².
The property features three bedrooms and one bathroom
It sits on a 389 m² block of land
Yes, the home comes with one parking space for a vehicle
Beau and Jessi Park is about 0.4 km away and Gordonvale Park is roughly 0.8 km from the house
Banks has a small shopping centre on Pockett Avenue that includes a SUPAEXPRESS supermarket, two takeaway food shops and a pet grooming shop
The Rob Roy Nature Reserve lies to the east of Banks, and the nearby Big Monks mountain offers a gliding stage for paragliders
The surface geology is alluvium, while the surrounding hills are composed of Silurian‑age Deakin Volcanics
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