22 Wilson Crescent
22 Wilson Crescent, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jul 2014 | $385,000 | $648 |
| Sold | Apr 2009 | $375,000 | $631 |
| Sold | Aug 2003 | $267,000 | $449 |
| Sold | Nov 1998 | $110,000 | $185 |
| Sold | Jan 1995 | $118,000 | $198 |
Price per m² based on land size of 594 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714852935
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/58/10
- Remoteness area
- Metro
- Property type
- House
- Land size
- 594 m²
- Internal area
- -
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Real Estate Agencies
Frequently asked questions
How many bedrooms and bathrooms does the house have?
The property features three bedrooms and one bathroom, providing comfortable accommodation for a small family or couple.
What is the size of the land parcel?
The house sits on a 594 m² block, offering a modest yard for gardening or outdoor activities.
What parking facilities are available at the property?
The home includes two designated parking spaces for residents and guests.
Which parks are located close to 22 Wilson Crescent?
Beau and Jessi Park is just about 0.2 km away, and Gordonvale Park is roughly 1 km to the south, both within easy walking distance.
Where is the nearest shopping centre and what does it offer?
A small shopping centre on Pockett Avenue is a short walk from the property and includes a SUPAEXPRESS supermarket, two take‑away food outlets and a pet grooming shop.
What natural attractions are near the suburb of Banks?
To the east lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the nearby Big Monks hill offers a gliding stage for paragliders and hang‑gliders.
What geological features characterize the Banks area?
The surface geology consists of alluvium, while the surrounding hills are formed from Deakin Volcanics that erupted in the Silurian period, about 414 million years ago.