37 Troughton Street
37 Troughton Street, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2001 | $213,000 | $284 |
| Sold | May 1994 | $160,000 | $213 |
| Sold | Mar 1993 | $48,500 | $64 |
Price per m² based on land size of 748 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714851155
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/64/27
- Remoteness area
- Metro
- Property type
- House
- Land size
- 748 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 37 Troughton Street?
It is a standalone house offering spacious living within the Banks suburb of Canberra.
How many bedrooms and bathrooms does the property have?
The home features four bedrooms and two bathrooms, providing ample accommodation for a family.
What is the size of the land on which the house sits?
The property sits on a 748 m² block, giving room for a garden or outdoor activities.
What parks are within walking distance of 37 Troughton Street?
Beau and Jessi Park is about 0.5 km away and Gordonvale Park is roughly 1.3 km distant, both offering green space for recreation.
Is there a local shopping centre near the property?
Yes, a small shopping centre on Pockett Avenue, containing a SUPAEXPRESS supermarket, take‑away food shops, and a pet grooming salon, is located a short distance away in Banks.
What natural attractions are located to the east of the suburb?
The Rob Roy Nature Reserve, part of Canberra Nature Park, lies east of Banks, and the nearby Big Monks mountain offers a gliding stage for paragliders and hang‑gliders.
What is the underlying geology of the Banks area?
The surface geology is alluvium, while the surrounding hills are composed of Deakin Volcanics, volcanic rocks formed during the Silurian age about 414 million years ago.