22 Smeaton Circuit
22 Smeaton Circuit, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Sep 2002 | $225,000 | $285 |
| Sold | Sep 2001 | $179,950 | $228 |
| Sold | Jan 1994 | $126,000 | $159 |
| Sold | Dec 1993 | $48,500 | $61 |
Price per m² based on land size of 788 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714854693
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/45/30
- Remoteness area
- Metro
- Property type
- House
- Land size
- 788 m²
- Internal area
- -
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Real Estate Agencies
Nearby schools
Frequently asked questions
What type of dwelling is located at 22 Smeaton Circuit?
22 Smeaton Circuit is a standalone house. It sits on a generous block of land.
How large is the land parcel for this property?
The house is set on 788 m² of land, providing ample outdoor space.
Which parks are closest to the property?
Beau and Jessi Park is about 0.5 km away, Gordonvale Park is roughly 1.3 km distant, and the local Banks Oval is within the suburb itself, about 0.3 km from the house.
What shopping amenities are available nearby?
A small shopping centre on Pockett Avenue serves the area, offering two take‑away food shops, a pet grooming shop and a SUPAEXPRESS supermarket.
What natural attractions are situated east of the property?
To the east lie the Rob Roy Nature Reserve, part of Canberra Nature Park with Mt Rob Roy, and the smaller mountain Big Monks, which features a gliding stage for paragliders and hang‑gliders.
How is the suburb of Banks geographically defined?
Banks is bounded by Box Hill Avenue, Tom Roberts Avenue and Tharwa Drive, and it slopes gently to the west‑northwest.
What is the underlying geology of the Banks area?
The surface geology is alluvium, while the surrounding hills are composed of Deakin Volcanics that erupted during the Silurian age, about 414 million years ago.