Richardson 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.
It is a stand‑alone house featuring four bedrooms and sits on a 946 m² block of land
The property encompasses 946 m² of land, providing ample space for a garden, outdoor entertaining or future extensions
Tuggeranoff Creek lies about 0.3 km away, offering a nearby natural water feature within walking distance
ACTION bus routes 74, 75, 76 and 78 serve Richardson, linking the area to Tuggeranoff Town Centre, Erindale Centre and neighbouring suburbs
Richardson was gazetted on 5 May 1975 and is named after novelist Ethel Florence Lindesay Richardson, with streets honouring writers, especially female authors
Within 1 km you’ll find the Richardson local centre and Oval on May Gibbs Close, the Tuggeranoff Homestead heritage site (≈0.7 km), and the neighbouring suburbs of Calwell, Gowrie and Isabella Plains
The suburb is covered by Quaternary alluvium, formed from erosion of surrounding Deakin Volcanics, while deeper layers consist of Silurian‑age volcanic rocks dating back about 414 million years
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