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.
It is a detached house situated on a 384 m² block of land
The residence is about 0.7 km from the heart of Dunlop
The property is near Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, with The Boslem and Harte Park about 2 km away and Goodwin Hill roughly 1.2 km distant
Fraser, Charnwood (around 2 km) and Macgregor (about 1.4 km) lie close to the home, all forming part of the Belconnen district
At the 2016 census Dunlop had 7,197 residents with a median age of 33 years, younger than the national median of 38
For federal elections Dunlop is in the division of Fenner, and for ACT Legislative Assembly elections it falls within the Ginninderra electorate
The suburb sits on Silurian‑age rocks, predominantly 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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