Kaleen ACT 2617, 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 at 11 Loddon Street is a standalone house
The land size for the house is 847 m²
There are two small shopping centres on Maribyrnong Avenue and a larger centre on Georgina Crescent near Kaleen’s border. Kaleen Plaza is also about 1 km away
Fern Hill Park is approximately 1.6 km from the property, and the suburb features several ovals such as Kaleen North and South ovals. The Lyneham Ridge eucalypt plantation lies on the eastern side of Kaleen
All Saints Greek Orthodox Church is about 0.9 km away, and other churches line Georgina Crescent within the suburb
The Royal Australian Naval Transmitting Station, a historic Commonwealth heritage site, is roughly 0.5 km away, and the Synemon Plana moth habitat is about 1.1 km distant
The eastern part of Kaleen sits on Silurian‑age calcareous shale of the Canberra Formation, while the western side consists of Ordovician greywacke from the Pittman Formation. These two units are separated by the Gungahlin Fault
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