4 Opal Street
4 Opal Street, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jun 2005 | $380,600 | $723 |
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.
- GAACT714852197
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/36/32
- 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 is the size of the land that the house at 4 Opal Street sits on?
The property occupies a land area of 526 m². This provides ample space for a garden or outdoor activities.
What type of dwelling is located at 4 Opal Street?
4 Opal Street is a standalone house. It is situated within the residential neighbourhood of Banks.
Which parks are closest to 4 Opal Street?
Beau and Jessi Park is about 0.2 km away, and Gordonvale Park is roughly 0.8 km from the house. Both parks offer open green space for recreation.
Is there a local shopping centre near the property?
Yes, a small shopping centre on Pockett Avenue is within the suburb, featuring a SUPAEXPRESS supermarket, two take‑away food shops and a pet grooming shop.
What natural reserves or outdoor features are near Banks?
The Rob Roy Nature Reserve lies to the east of Banks, offering hilly terrain and the views of Mt Rob Roy. A smaller mountain, Big Monks, is also nearby and is popular with paragliders and hang‑gliders.
What community facilities are available in Banks?
Banks Oval, the suburb’s only oval, is used for local events such as Little Athletics and school athletics carnivals. It provides a focal point for community sport and gatherings.
What is the geological makeup of the area around 4 Opal Street?
The surface geology of Banks is alluvium, while the surrounding hills are composed of Deakin Volcanics that erupted during the Silurian age, about 414 million years ago.