Fadden ACT 2904, 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.
It is a standalone house situated on a residential block
The parcel of land measures approximately 930 m²
ACTION bus routes 74 and 75 operate a circular service linking Fadden and nearby suburbs with Tuggeranong Town Centre and Erindale Centre, while route 76 connects Fadden, Gowrie and Macarthur to those same centres
Residents are within a short walk of Hannah Community Park (about 1 km) and Wanniassa Hills Nature Reserve (around 1‑2 km), and the Fadden Pine Plantation with playgrounds and barbecues is also nearby
The Fadden local shopping centre on Hanlon Crescent provides a hairdresser, medical centre, chiropractor, massage therapist and a veterinary hospital. The suburb also features the Fadden Neighbourhood Oval, tennis courts off Stopford Crescent, and the MacArthur Scout Hall on Coyne Street
The eastern part of Fadden sits on alluvial deposits, while the western side consists of Deakin Volcanics rhyolite from the Silurian age, which can appear green‑grey, purple or cream, and a fault with a quartz outcrop runs north‑north‑west from MacArthur Hill
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