Wanniassa ACT 2903, 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 features four bedrooms. All rooms are part of a standalone house on the site
The house sits on a 1,202 m² block. This provides ample space for outdoor activities and landscaping
The Wanniassa Observatory is approximately 0.6 km away, making it a short walk from the home
Erindale Centre, a major shopping complex, is about 1.3 km from the property. It offers a range of retail and service outlets
Viking Park, a local stadium, is roughly 1.4 km away, and the Farrer Ridge Nature Reserve is also about 1.4 km from the site, providing opportunities for sports and nature walks
Wanniassa is serviced by several ACTION bus routes, including the R5 and routes 72‑77, which connect to the Erindale Interchange and the wider Canberra region
The suburb sits on Deakin Volcanics from the Silurian period, about 414 million years old, comprising cream‑green and purple rhyodacite in the east and tuff, agglomerate, and rhyolite in the west
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