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 | 24 Jun 2003 | $285,000 | $716 |
| Sale | 5 Mar 1997 | $139,000 | $349 |
| Sale | 17 Jan 1995 | $44,000 | $110 |
Price per m² based on land size of 398 m².
It is a standalone house situated on a 398 m² block in the suburb of Ngunnawal
The home features three bedrooms and two bathrooms
The house sits on a land area of 398 square metres
The property includes two allocated parking spaces
Ngunnawal is approximately 4 km from the Gungahlin Town Centre and about 13 km from the centre of Canberra
Nearby parks include Ginninderra Park (≈0.6 km), Crinigan Park (≈0.6 km), Violets Park (≈0.7 km) and Girrawah Park (≈0.9 km)
Ngunnawal rests on the Canberra Formation, primarily composed of slaty shale and mudstone, with outcrops of dacite, quartz‑andesite, tuff, and ashstone shaped by north‑northeast folds and the nearby Deakin Fault
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