Flynn ACT 2615, 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 offering three bedrooms. The property sits on a generous 709 m² block
The land area measures 709 m², providing ample outdoor space for gardening, recreation, or future development
George Simpson Park is just 0.3 km away, and The Boslem and Harte Park lies about 1.2 km from the home, both offering green space and walking paths
The residence is situated roughly 1 km from the heart of Flynn, making local shops and services easily accessible
Flynn is positioned between Tillyard Drive, Kingsford Smith Drive and Ginninderra Drive, providing good arterial connections to the rest of Canberra
Federally, the property falls within the Division of Fenner, while for ACT Legislative Assembly elections it is part of the Ginninderra electorate
The southwest part of Flynn is dominated by Deakin Volcanics purple rhyodacite, with grey rhyodacitic tuff and green‑grey rhyodacite in the south, and the Deakin Fault separating these from the Hawkins Volcanics in the north‑east
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