18 House Circuit
18 House Circuit, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2001 | $145,000 | $310 |
| Sold | Dec 1996 | $110,098 | $235 |
| Sold | May 1992 | $102,000 | $218 |
Price per m² based on land size of 467 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714850368
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/5/48
- Remoteness area
- Metro
- Property type
- House
- Land size
- 467 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 property is located at 18 House Circuit?
It is a detached house situated on a 467 m² block of land.
How large is the land parcel for the house?
The land area is 467 square metres, providing space for a garden or outdoor amenities.
What is the character of the Banks suburb where the property is located?
Banks is Canberra’s most southerly suburb, named after botanist Sir Joseph Banks, and features gently sloping terrain with street names themed around botany and natural history.
Which parks are within walking distance of the home?
Beau and Jessi Park and Gordonvale Park are both about 0.4 km away, offering green space and recreational options.
What shopping facilities are available nearby?
A small local shopping centre on Pockett Avenue includes a SUPAEXPRESS supermarket, two take‑away food shops, and a pet grooming service, all within the suburb.
Are there any natural reserves or landmarks close to the property?
The Rob Roy Nature Reserve lies to the east of Banks, and the nearby Big Monks mountain provides a gliding stage for paragliders and hang‑gliders.
What is the geological makeup of the Banks area?
The surface geology of Banks consists of alluvium, while the surrounding hills are formed from Deakin Volcanics, volcanic rocks dating back to the Silurian period about 414 million years ago.