Dunlop ACT 2615, 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 | 4 Apr 1994 | $58,000 | $84 |
Price per m² based on land size of 687 m².
The property sits on a 687 m² block of land
Dunlop is located about 11.6 km north‑west of Canberra’s city centre, so the house is roughly that distance from downtown
The suburb borders the Dunlop Grasslands Nature Reserve and includes West Belconnen Ponds, Jarramlee Pond and Fassifern Pond within the Ginninderra Catchment. The Boslem and Harte Park is also about 1 km away
Kippax Fair Shopping Centre and the nearby Kippax Centre are both approximately 2.3 km from the home, offering a range of retail options
The National Health Co‑op Kippax branch is situated about 2.3 km away, providing convenient health services
Dunlop rests on Silurian‑age rocks, mainly Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west. The Deakin Fault runs along the north‑east edge, and the Hawkins Volcanics (green‑grey dacite and quartz‑andesite) are uplifted on the north‑east side
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