Campbell ACT 2612, 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.
18 Wells Road is a standalone house situated within the suburb of Campbell
The residence sits on an expansive 695,174 m² block, providing ample space for private landscaping or development
The house is within walking distance of several heritage sites, including Duntroon (0.1 km) and the Royal Military College (0.3 km), as well as a number of historic Commonwealth heritage assets clustered between 0.3 km and 0.5 km away
Campbell is bounded to the south‑east by the Mount Pleasant Nature Reserve, and Daley Park on Ferdinand Street, featuring mature native trees and a small playground, are both a short distance from the property
At the 2021 census Campbell had 6,564 residents, with 70.5 % born in Australia. The most common responses for religion were No Religion (48.9 %), Catholic (17.8 %) and Anglican (8.3 %)
The suburb sits on the lowest layer of the Ainslie Volcanics, a grey dacite formation, with additional layers of grey quartz andesite and cream rhyolite in the north‑east, all formed during the Silurian period
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