35 Wilhelmi Crescent
35 Wilhelmi Crescent, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jan 2022 | $698,000 | $1,789 |
Price per m² based on land size of 390 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714890392
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/13/37
- Remoteness area
- Metro
- Property type
- House
- Land size
- 390 m²
- Internal area
- 93 m²
- 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 dwelling is located at 35 Wilhelmi Crescent?
It is a standalone house offering three bedrooms and one bathroom, suitable for a small family or couple.
How many parking spaces are provided with the property?
The residence includes two dedicated parking spaces for residents' vehicles.
What shopping options are close to the home?
A small shopping centre on Pockett Avenue is nearby, featuring a SUPAEXPRESS supermarket, two take‑away food outlets, and a pet grooming shop.
Which parks and recreational areas can be found within walking distance?
Beau and Jessi Park, Gordonvale Park and the local Banks Oval – used for Little Athletics and community events – are all within about a kilometre of the address.
What natural reserves or landscape features are near the property?
To the east lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the smaller mountain Big Monks with a gliding stage is also accessible nearby.
How far is the property from the centre of Banks and the neighbouring suburb of Conder?
The home is roughly 0.8 km from the centre of Banks and about 0.9 km from Conder, making local services easily reachable.
What is the geological makeup of the Banks area surrounding the house?
The surface geology consists of alluvium, while the surrounding hills are formed from Deakin Volcanics that erupted in the Silurian period, around 414 million years ago.