Kambah ACT 2902, 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.
The property is a standalone house situated on a 326 m² land parcel
Kambah is Canberra’s northernmost Tuggeranong suburb, the largest in area (about 1130 ha) and primarily composed of detached single‑storey homes, bordered by Mount Taylor and the Canberra Nature Park
Nearby amenities include the Murrumbidgee Country Club, three district playing fields, a tennis club, the Kambah Pony Club, Vikings BMX Park, and two Scout halls within the suburb
Tuggeranong United FC, a local football club, is approximately 1.1 km from the property
The home is close to Urambi Hill (about 1.5 km) and Mount Taylor (around 2‑3 km), and the western side of Kambah borders the Murrumbidgee River with its Red Rocks Gorge and Kambah Pool swimming hole
Kambah rests on Silurian volcanics, mainly grey rhyodacitic and dacitic crystal tuff of the Laidlaw Volcanics, with additional rhyolite, porphyry intrusions and older Deakin Volcanics found on surrounding hills
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