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 | 31 Aug 1992 | $71,500 | $89 |
Price per m² based on land size of 801 m².
It is a standalone house situated on a large 801 m² block, providing a spacious residential setting
The land measures 801 m², offering plenty of room for a garden, outdoor entertainment or future extensions
18 Macedon Crescent is in the suburb of Palmerston, part of the Gungahlin district, bounded by Gungahlin Drive and Gundaroo Drive and close to Nicholls, Gungahlin, Crace and Franklin
ACTION bus routes 21, 22, 23 and 24 travel along Kosciuszko Avenue and through Palmerston, connecting the area to Gungahlin Town Centre, Franklin and Nicholls
George Kemp Park is about 0.8 km away and Girrawah Park roughly 1.6 km away, both offering open space for walking, picnics and community activities
Palmerston sits on the late‑middle Silurian Canberra Formation, mainly slaty shale and mudstone, with a distinctive ashstone exposure shaped like an ear of corn and intersected by faults such as the Winslade and Gungahlin faults
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