Richardson ACT 2905, Australia
Key points for 24 Baynton Street.
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 three bedrooms. All bedrooms are within the main house structure
The home sits on a block of approximately 829 m². This provides ample outdoor space around the house
It is a stand‑alone house. The residence is a typical suburban home within Richardson
ACTION bus routes 74, 75 and 76 connect the suburb to Tuggeranong Town Centre and Erindale Centre, while route 78 provides service to Tuggeranong Town Centre via Isabella Plains and Bonython
Tuggeranong Creek is just about 0.4 km away, and the Tuggeranong Homestead heritage site can be reached within roughly 0.6 km. The Richardson local centre and Richardson Oval are also nearby on May Gibbs Close
Richardson was gazetted as a suburb on 5 May 1975. It is part of the Tuggeranong district in Canberra
The suburb is covered by Quaternary alluvium, formed from erosion of surrounding volcanic rocks. Beneath this layer lie Silurian‑age volcanic rocks dating back about 414 million years
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