Campbell ACT 2612, 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 | 11 Jul 2009 | $815,000 | $806 |
| Sale | 19 Aug 2005 | $610,000 | $603 |
Price per m² based on land size of 1010 m².
The property sits on 1,010 m² of land, providing ample space for a garden or outdoor activities
The house features four bedrooms and one bathroom, suitable for a family household
The Australian Defence Force Academy is about 0.6 km away and UNSW Canberra is roughly 0.7 km away, both within easy walking distance
Nearby parks include Victoria Cross Park (≈0.8 km), Legacy Park (≈0.8 km), George Cross Park (≈0.9 km) and RSL Park (≈1.0 km), offering convenient green space
Mount Pleasant is approximately 0.8 km from 44 Gellibrand Street, providing nearby natural scenery
Campbell rests mainly on the lowest layer of the Ainslie Volcanics, made up of grey dacite, agglomerate and tuff, with higher layers of grey quartz andesite to the north and cream rhyolite to the northeast, all formed in the Silurian period
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