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.
The property at 1 Stubbs Crescent is a standalone house. It is situated within the residential neighbourhood of Theodore
The house sits on a land area of 972 m². This provides ample space for a garden or outdoor amenities
Sacred Heart Church in the neighbouring suburb of Calwell is about 0.5 km away, making it a short walk from the house
The suburb borders the Tuggeranong Hill nature reserve, and the hill itself is roughly 2 km from 1 Stubbs Crescent, offering easy access to trails and native bushland
The suburb of Theodore is bounded by the Monaro Highway, giving the property convenient road connectivity to the rest of Canberra
Theodore is named after Edward Granville Theodore (1884–1950), who served as Queensland premier and deputy Prime Minister of Australia. The name was officially gazetted on 5 August 1975
The land beneath Theodore consists of Deakin Volcanics, including various rhyodacite and rhyolite deposits from the Late Silurian period (about 414 million years ago). These volcanic rocks are interspersed with Quaternary alluvium in the lower northern parts
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