Lyneham ACT 2602, 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 situated on a sizeable block in Lyneham
The property sits on approximately 792 m² of land, offering ample outdoor space
The Old Canberra Inn is about 0.8 km away, Tilley's café is roughly 1.2 km distant, and the National Hockey Centre is just 1.0 km from the house
Lyneham is serviced by five light‑rail stops on its eastern edge, including Macarthur Avenue and Dickson Interchange, and by several bus routes such as R9, 30, 31, 50 and 51
Yes, the National Hockey Centre is about 1.0 km away, and the suburb also hosts facilities like the ACT Netball Centre and Thoroughbred Park within short driving distance
Lyneham features leafy streets, bushland reserves, and a scenic wetland near Sullivans Creek that provides wildlife habitat and walking trails
The suburb sits on Silurian calcareous shales from the Canberra Formation overlain by Quaternary alluvium, with Ordovician greywacke present in the north‑west
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