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 | 19 Feb 1998 | $41,500 | $81 |
Price per m² based on land size of 511 m².
9 Marchant Circuit is a standalone house situated on a residential lot
The house sits on a 511 m² parcel of land, providing a modest yard surrounding the residence
It is in the suburb of Dunlop, part of the Belconnen district, roughly 11–12 km north‑west of Canberra’s city centre
Nearby green spaces include the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond, Fassifern Pond, The Boslem And Harte Park (about 1.6 km away) and George Simpson Park (approximately 2 km away)
Halls Creek runs about 1.2 km from the house, offering a natural watercourse within easy reach
Dunlop is adjacent to the suburbs of Fraser, Charnwood and Macgregor, all located within a 2–3 km radius
The suburb sits on Silurian‑age rocks, primarily Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west and the Deakin Fault along its north‑east edge
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