Amaroo ACT 2914, 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 | 3 Apr 2002 | $310,000 | $275 |
| Sale | 14 Jul 1999 | $48,000 | $42 |
Price per m² based on land size of 1127 m².
10 Geehi Place is a standalone house featuring five bedrooms
The house sits on a 1,127 m² block, providing ample outdoor space
Amaroo is approximately 15 km from the centre of Canberra and about 1.4 km from the Gungahlin Town Centre
In the Nyoongar language, “Amaroo” translates to “a beautiful place”
Within roughly 0.5–1.6 km you’ll find Crinigan Park, Violets Park, Ginninderra Park, Homestead Park, and Yerrabi Pond
Yes, the historic Crinigan’s Hut Ruin lies about 0.5 km away, and the area includes the remains of Crinigan’s stone cottage from the 1840s
Amaroo sits on the late middle Silurian Canberra Formation, primarily composed of slaty shale and mudstone, with bands of dacite, quartz‑andesite, and a fault line running along Ginninderra Creek
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