20 Wilhelmi Crescent
Banks ACT 2906, Australia
Snapshot
Key points for 20 Wilhelmi Crescent.
- Courtyard home with mature, low‑maintenance gardens and established trees
- Double‑length, extra‑wide garage plus single carport provide three parking spaces
- Three bedrooms; two feature built‑in wardrobes, separated from main living area
- G‑shaped kitchen maximizes storage and utilizes every square inch
- Open‑plan living flows to an expansive raised pergola and deck
Key details
- Locality
- Banks
- State
- ACT
- Coordinates
- 35.4651501 / 149.09628451
- GNAF PID
- GAACT714900799
- Legal parcel ID
- TUGG/BANK/14/37
- Remoteness area
- Metro
- Property type
- House
- Land size
- 416 m²
- Land Use Category
- Residential
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sale | 29 Sep 2015 | $368,000 | $884 |
Price per m² based on land size of 416 m².
Real Estate Agencies
Nearby schools
Frequently asked questions
How many bedrooms and bathrooms does 20 Wilhelmi Crescent have?
The property features three bedrooms and one bathroom
What type of dwelling is 20 Wilhelmi Crescent?
It is a standalone house located in the suburb of Banks, ACT
What parking provision does the property offer?
The home includes three parking spaces for resident use
Which parks are within walking distance of the property?
Beau and Jessi Park and Gordonvale Park are both about 0.5–0.7 km away, providing nearby green space
What shopping facilities are close to the property?
A small shopping centre on Pockett Avenue offers a SUPAEXPRESS supermarket, two take‑away food shops, and a pet grooming shop
What natural reserves or landmarks are near Banks?
To the east lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the smaller mountain Big Monks, which is accessible from nearby Wollemi Place
Why is the suburb named Banks?
The suburb is named after Sir Joseph Banks, the botanist who accompanied Captain James Cook to Botany Bay in 1770
What is the underlying geology of the Banks area?
The surface geology is alluvium, while the hills are formed from Deakin Volcanics that erupted during the Silurian period about 414 million years ago
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