Palmerston ACT 2913, 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 | 22 Apr 1992 | $60,500 | $49 |
Price per m² based on land size of 1227 m².
The property occupies 1,227 m² of land
It is situated in the suburb of Palmerston, ACT, which is bounded by Gungahlin Drive and Gundaroo Drive and lies near the suburbs of Nicholls, Gungahlin, Crace and Franklin
ACTION bus routes 21, 22, 23 and 24 run along Kosciuszko Avenue and through parts of Palmerston, providing connections to Gungahlin Town Centre, Franklin and Nicholls
George Kemp Park is about 1.1 km away, Ginninderra Park is roughly 1.9 km distant, and Girrawah Park can be reached in about 2 km
The Gungahlin Enclosed Oval and the Gungahlin United Football Club are each approximately 1.8 km from the house, offering sports and community events
Palmerston sits on the Canberra Formation from the late middle Silurian age, comprising slaty shale, mudstone and a distinctive ashstone exposure shaped like an ear of corn, with associated anticlines, synclines and faults such as the Winslade and Gungahlin faults
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