38 Bastow Circuit
38 Bastow Circuit, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Sep 2002 | $193,000 | $362 |
| Sold | Nov 2000 | $135,000 | $253 |
| Sold | Sep 1992 | $107,500 | $202 |
| Sold | May 1992 | $26,000 | $48 |
Price per m² based on land size of 532 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714852032
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/5/18
- Remoteness area
- Metro
- Property type
- House
- Land size
- 532 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 38 Bastow Circuit?
38 Bastow Circuit is a standalone house. It sits on a residential lot within the suburb of Banks, Canberra.
How much land does the property at 38 Bastow Circuit occupy?
The house sits on a 532 m² block of land. The site is part of the alluvial surface that characterises the whole suburb.
Which parks are closest to 38 Bastow Circuit?
Gordonvale Park is about 0.3 km away, while Beau and Jessi Park is roughly 0.6 km distant. Both provide nearby green space for recreation.
What shopping facilities are available near the property?
A small shopping centre on Pockett Avenue serves the area, featuring two take‑away food outlets, a pet grooming shop and a SUPAEXPRESS supermarket. It is within easy walking distance for residents.
What natural features or reserves are located near Banks?
To the east of Banks lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the smaller mountain Big Monks, which offers a gliding stage for paragliders. Both are accessible from nearby streets.
What is the geology of the land on which 38 Bastow Circuit is built?
The surface geology of the entire suburb, including the property, is alluvium. Beneath this lie the Deakin Volcanics, volcanic rocks that formed during the Silurian age about 414 million years ago.