Bruce ACT 2617, 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 sits on a 2,048 m² block, providing ample space for the house and outdoor activities
Fern Hill Park is located about 0.4 km from the house, making it a very short walk for easy access to green space
Canberra Stadium and the Australian Institute of Sport are each roughly 1 km away, offering opportunities to attend rugby matches and other sporting events
Bus routes R2, R3, R4 and R9 run through Bruce, connecting the suburb to the University of Canberra, Calvary Hospital, and the Gungahlin light rail at Dickson
The University of Canberra is approximately 1.1 km from 101 Norman Fisher Circuit, within easy walking or cycling distance
Bruce was gazetted on 6 June 1968 and is named after Viscount Bruce of Melbourne, the eighth Prime Minister of Australia and first Chancellor of the Australian National University
Bruce is primarily composed of greywacke from the Ordovician Pittman Formation, with bands of black Acton Shale and Silurian-age adamellite intrusions across the area
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