Hughes ACT 2605, 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.
The property features five bedrooms and three bathrooms, offering ample space for a family
The home sits on a block of approximately 859 m², providing a generous outdoor area
The listing includes two parking spaces for resident use
Hughes offers the North Woden Tennis Club, Clarrie Hermes Park (Hughes Oval), three local playgrounds, and walking trails that lead toward the Federal Golf Course and Red Hill Nature Reserve
Nature Park is located about 0.6 km away, providing easy access to green space
Hughes is named after former Prime Minister William Morris “Billy” Hughes, was gazetted on 20 September 1962, and saw residential construction begin in 1963, growing to a population of over 4,000 by 1974
The suburb contains shale from the Yarralumla Formation in the south‑west, cream‑coloured rhyolite from the Mount Painter Volcanics in the north‑west, dark purple rhyodacite from the Deakin Volcanics to the north, and a tuff layer in the south‑east, with an inactive fault running through the area
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