Theodore ACT 2905, 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.
46 Tewksbury Circuit is a standalone house. It sits on a single residential lot within the suburb of Theodore
The property occupies approximately 1,235 m² of land. This size provides space for a garden, outdoor entertaining or future extensions
Theodore is bounded by the Monaro Highway and Tharwa Drive. These arterial roads provide convenient access to the surrounding Canberra region
The property is near Tuggeranong Hill and the Canberra Nature Park of Tuggeranong Hill nature reserve, both within roughly 2 km. These areas offer walking trails and natural scenery
On the north‑eastern side of Theodore are the Theodore Grinding Grooves, a rare Aboriginal artefact site valued by the Ngunnawal people. The site demonstrates historic Aboriginal grinding techniques
The suburb rests on Deakin Volcanics, including rhyodacite and rhyolite formations from the late Silurian period (about 414 million years ago). These volcanic rocks underlie most of the land in the area
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