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.
The property is a single‑storey house that sits on a 685 m² block and includes four bedrooms and two bathrooms
The Fadden local shopping centre on Hanlon Crescent, which houses a hairdresser, medical centre, chiropractor, massage therapist and a veterinary hospital, is located within the suburb and can be reached on foot from the property
Hannah Community Park is about 0.7 km away, the Fadden Pine Plantation offers playgrounds and barbecues a short drive away, and Wanniassa Hills Nature Reserve is roughly 1.8 km from the house
ACTION bus routes 74 and 75 run a circular service connecting Fadden with the Tuggeranong Town Centre and Erindale Centre, while route 76 links the suburb to Erindale Centre and the wider Tuggeranong area
The eastern part of Fadden is built on alluvium, while the western side sits on Deakin Volcanics rhyolite that can appear green‑grey, purple or cream and dates back to the Silurian period; a fault with a quartz outcrop trends north‑north‑west from Macarthur Hill
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