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 | 31 Oct 2020 | $763,000 | $937 |
| Sale | 24 Mar 2011 | $486,000 | $597 |
| Sale | 8 Nov 2002 | $95,000 | $116 |
| Sale | 23 Apr 2002 | $86,000 | $105 |
Price per m² based on land size of 814 m².
The property features three bedrooms and two bathrooms
It sits on an 814 m² block, providing ample outdoor space
The home includes two parking spaces for residents
The Boslem And Harte Park is about 0.8 km away, offering nearby green space
Dunlop Grasslands Nature Reserve and the West Belconnen Ponds are within the suburb, and Goodwin Hill is roughly 1.5 km to the north‑east
The suburb of Dunlop is approximately 11.6 km north‑west of Canberra’s city centre
The area sits on Silurian‑age rocks, mainly Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west and the Deakin Fault running along the north‑east edge
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