2 West Place
2 West Place, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Built | Unknown | — |
Price per m² based on land size of 922 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714850325
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/52/16/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 922 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
What type of dwelling is located at 2 West Place?
2 West Place is a standalone house offering three bedrooms and one bathroom. It sits on a generous 922 m² block, providing ample outdoor space.
How large is the land parcel for this property?
The property occupies 922 m² of land, giving owners plenty of room for gardens, recreation or future development within the suburb.
What recreational facilities are close to the home?
The house is within walking distance of Beau and Jessi Park (about 0.5 km) and Gordonvale Park (around 1.4 km). The local Banks Oval, used for community sports and events, is also nearby.
What shopping amenities are available in Banks?
Banks features a small shopping centre on Pockett Avenue that includes a SUPAEXPRESS supermarket, two take‑away food shops, and a pet grooming outlet, all within the suburb.
What natural attractions are near the property?
To the east of Banks lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the nearby Big Monks mountain, which offers a gliding stage for paragliders and hang‑gliders.
When was the suburb of Banks established and what is its namesake?
Banks was gazetted on 12 March 1987 and is named after Sir Joseph Banks, the botanist who sailed with Captain James Cook to Botany Bay in 1770.
What is the underlying geology of the area?
The surface of Banks is covered by alluvium, while the surrounding hills are composed of Deakin Volcanics, a Silurian‑age volcanic formation about 414 million years old.