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.
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sale | 7 Feb 2025 | $840,000 | $1,206 |
| Sale | 31 May 1993 | $60,000 | $86 |
Price per m² based on land size of 696 m².
The property sits on a 696 m² block, providing ample space for a family home and outdoor activities
The home offers four bedrooms and two bathrooms, suitable for a medium‑sized household
The residence includes two dedicated parking spaces for residents and guests
Violets Park is just about 0.2 km away, Homestead Park is roughly 0.3 km, and Gold Creek Park is within 0.7 km, making green spaces easily accessible
The Arabanoo Street Library is located nearby, and the historic Gold Creek Homestead is about 0.5 km from the home, offering cultural and educational amenities
Ngunnawal sits on the Canberra Formation, primarily composed of slaty shale and mudstone, with dacite and quartz andesite in the north‑west corner and various tuff and ashstone exposures. These rock formations were shaped by folding aligned north‑north‑east and the nearby Deakin Fault runs parallel to the fold axes
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