Reid 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.
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sale | 16 Oct 1998 | $293,000 | $441 |
| Sale | 5 Jul 1990 | $177,000 | $266 |
Price per m² based on land size of 663 m².
The property sits on a 663 m² block of land
Anzac Parade is about 0.5 km away, a short walk from the house
Glebe Park is approximately 0.3 km from the house, offering nearby green space for recreation
The Canberra Institute of Technology is roughly 0.3 km away, within easy walking distance
The National Convention Centre, Crowne Plaza Canberra hotel, and Casino Canberra are each about 0.4 km from the house
Reid is one of Canberra’s oldest suburbs, established in the 1920s for public servants and featuring heritage‑listed sites such as St John the Baptist Church, which dates back to 1845
The suburb rests on calcareous shale from the Canberra Formation, overlain by Quaternary alluvium and nearby pebbly gravels left from an earlier, higher Molonglo River
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