Ngunnawal ACT 2913, 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 home features three bedrooms. It is a standalone house set on a 361 m² block
The property occupies 361 m² of land. This provides space for a garden or outdoor entertaining area
It is situated roughly 4 km from the Gungahlin Town Centre, making shops and services easily reachable by car or bus
The suburb of Ngunnawal lies about 13 km from the centre of Canberra, a short drive to the city’s main attractions and amenities
Gold Creek Homestead is just 0.1 km away and Homestead Park is about 0.3 km from the property, both offering nearby green space and historic interest
Ngunnawal is named in tribute to the Ngunnawal people, the original inhabitants of the area. The suburb was officially gazetted on 24 April 1992
The area sits on the Canberra Formation, mainly composed of slaty shale and mudstone, with pockets of dacite, quartz‑andesite, and tuff. These rock types were laid down in the late middle Silurian age and have been studied for their folding patterns and fault lines
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