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 | 1 Sep 2004 | $325,000 | $647 |
| Sale | 18 Jul 2002 | $240,000 | $478 |
| Sale | 16 Mar 2000 | $153,900 | $306 |
| Sale | 11 Aug 1999 | $41,500 | $82 |
Price per m² based on land size of 502 m².
The house features four bedrooms and two bathrooms
7 Hobday Place sits on a 502 m² block of land
It is located in the suburb of Dunlop, part of the Belconnen district, about 11.6 km north‑west of Canberra’s city centre
The property is close to the Dunlop Grasslands Nature Reserve and the West Belconnen, Jarramlee and Fassifern ponds, all part of the Ginninderra Catchment
The Boslem and Harte Park is approximately 1.5 km away, while George Simpson Park is about 2.4 km distant
Dunlop is adjacent to the suburbs of Fraser, Charnwood and Macgregor
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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