Chisholm ACT 2905, 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.
103 Clift Crescent is a house situated on an 827 m² block of land
Richardson is located approximately 0.4 km from the property, making it a very short walk
ACTION bus routes 74, 75, 76, 78 and 182 serve Chisholm, linking the area to Tuggeranong Town Centre, Erindale Centre and the Monaro Highway
Simpsons Hill, just over 1 km away, offers walking tracks popular for dog walking, and the suburb also includes the Chisholm District Playing Fields and The Pines Tennis Club
The Group Centre on Halley and Benham Streets provides a Coles supermarket, tavern, restaurants, a GP, dentist, BP service station, fire station, rugby union club and child‑care facilities
According to the 2021 census, Chisholm had 5,268 residents with a median age of 37, a median weekly household income of $2,292 and a median weekly personal income of $1,088
The suburb sits on Silurian‑age Deakin Volcanics, consisting of rhyolite throughout and rhyodacite around the eastern hill, with rocks displaying colours from cream to purple due to water alteration
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