8 Carter Place
8 Carter Place, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jun 1993 | $49,000 | $61 |
Price per m² based on land size of 803 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714854951
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/59/40
- Remoteness area
- Metro
- Property type
- House
- Land size
- 803 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 property is located at 8 Carter Place and how large is the land?
8 Carter Place is a house situated on a block of about 803 m². The property offers a spacious garden area typical of suburban homes in Banks.
Which parks are within a short walking distance of 8 Carter Place?
Beau and Jessi Park is only about 0.4 km away, and Gordonvale Park is roughly 1.2 km from the residence, both providing green space for recreation.
What shopping facilities are available nearby in Banks?
The suburb features a small shopping centre on Pockett Avenue, which includes a SUPAEXPRESS supermarket, two take‑away food shops, and a pet grooming shop.
What natural reserves or geographic features are situated east of the property?
East of Banks lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the nearby smaller mountain Big Monks, which has a gliding stage for paragliders and hang‑gliders.
How is the suburb of Banks geographically defined in terms of its boundaries and neighboring suburbs?
Banks is bounded by Box Hill Avenue, Tom Roberts Avenue and Tharwa Drive, and it adjoins the suburbs of Conder and Gordon, making it the most southerly suburb of Canberra.
What is the underlying geology of the area surrounding 8 Carter Place?
The surface geology of Banks is alluvium, while the surrounding hills are formed from Deakin Volcanics, volcanic rocks that erupted during the Silurian age about 414 million years ago.