25 Perrin Circuit
25 Perrin Circuit, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Nov 2025 | $938,000 | $1,221 |
| Sold | Sep 2022 | $880,000 | $1,145 |
| Sold | Apr 2016 | $472,000 | $614 |
| Sold | Jun 2010 | $485,000 | $631 |
| Sold | Jul 1992 | $35,000 | $45 |
Price per m² based on land size of 768 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714888661
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/15/60
- Remoteness area
- Metro
- Property type
- House
- Land size
- 768 m²
- Internal area
- 158 m²
- 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
How many bedrooms and bathrooms does the house at 25 Perrin Circuit have?
The property features three bedrooms and two bathrooms. It is a standalone house.
What is the size of the land the property occupies?
The house sits on a 768 m² block, providing a spacious yard within the suburb of Banks.
Does the property include parking facilities?
Yes, the home comes with two dedicated parking spaces for residents or guests.
Which parks are located close to 25 Perrin Circuit?
Beau and Jessi Park is about 0.5 km away and Gordonvale Park is roughly 0.7 km distant, both offering green space and recreation.
What shopping amenities are available in the Banks suburb?
Banks has a small shopping centre on Pockett Avenue that includes two takeaway food shops, a pet grooming shop, and a SUPAEXPRESS supermarket.
What natural reserves or scenic areas are near the property?
To the east of Banks lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the smaller mountain Big Monks, which features a gliding stage for paragliders.
What is the geological makeup of the Banks area?
The surface geology of Banks is alluvium, while the surrounding hills are composed of Deakin Volcanics that erupted during the Silurian period, about 414 million years ago.