Hackett 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.
The house sits on a 615 m² block. This provides ample space for a garden or outdoor entertainment area
6 Dakin Place is a standalone house. It forms part of the residential character of the Hackett suburb
Hackett lies approximately 4.5 km north‑east of Canberra’s CBD, placing the property within a short drive of the city centre
The home is near several green spaces, including Calvert Park (about 0.5 km away) and the Dickson Wetland (around 0.9 km). The suburb also borders the Mount Majura Nature Reserve to the east
St Margaret's Uniting Church is just 0.3 km away, and the Dickson Library can be reached within 1.7 km. Hackett also features a neighbourhood oval and a local shopping centre
The Officer Crescent bus shelter is located roughly 1 km from 6 Dakin Place, providing convenient access to Canberra’s bus network
Hackett sits on calcareous shales from the Canberra Formation, overlain by Quaternary alluvium. The higher eastern side rests on the lowest layer of the Ainslie Volcanics, composed of grey dacite and related volcanic material
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