31 Troughton Street
31 Troughton Street, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Oct 1993 | $108,000 | $205 |
| Sold | Mar 1993 | $36,500 | $69 |
Price per m² based on land size of 526 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714851019
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/64/30
- Remoteness area
- Metro
- Property type
- House
- Land size
- 526 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 31 Troughton Street?
31 Troughton Street is a detached house set on a 526 m² block of land. The residence offers the space of a typical suburban home in Banks.
How close is the nearest park to the property?
Beau and Jessi Park is the closest green space, situated about 0.5 km from the house. A slightly larger option, Gordonvale Park, lies roughly 1.3 km away.
What shopping amenities are available nearby?
A small shopping centre on Pockett Avenue serves the area, featuring a SUPAEXPRESS supermarket, two take‑away food shops, and a pet grooming business. Residents can reach it on foot within a few minutes.
Which natural attractions can be found near the property?
To the east of Banks lies the Rob Roy Nature Reserve, part of Canberra Nature Park, which includes Mt Rob Roy. The nearby Big Monks mountain offers a gliding stage popular with paragliders and hang‑gliders.
When was the suburb of Banks established and who is it named after?
Banks was officially gazetted on 12 March 1987. The suburb is named in honour of Sir Joseph Banks, the botanist who accompanied Captain James Cook to Botany Bay in 1770.
What is the geological makeup of the area around 31 Troughton Street?
The surface geology of Banks consists of alluvium deposits. Beneath this layer, the surrounding hills are formed from the Silurian‑age Deakin Volcanics, which erupted around 414 million years ago.