34 Ironbark Crescent
34 Ironbark Crescent, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jun 1997 | $135,000 | $133 |
| Sold | May 1992 | $131,200 | $130 |
| Sold | Mar 1992 | $33,500 | $33 |
Price per m² based on land size of 1009 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714853029
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/18/30
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1009 m²
- Internal area
- 159 m²
- 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 land size of the property at 34 Ironbark Crescent?
The house sits on a 1,009 m² block, providing ample outdoor space for gardens, recreation or future development.
How many bedrooms and bathrooms does the home offer?
The residence includes four bedrooms and two well‑appointed bathrooms, suitable for a family or guests.
What parking facilities are available at this address?
The property provides two dedicated parking spaces for residents and visitors.
Which parks are within easy walking distance of the home?
Beau and Jessi Park is just 0.2 km away, while Gordonvale Park is about 0.8 km from the house, both offering green space and playgrounds.
Are there any local shopping amenities nearby?
A small shopping centre on Pockett Avenue is nearby, featuring a SUPAEXPRESS supermarket, two takeaway food shops and a pet grooming service.
What natural features are close to Banks and the property?
To the east lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the smaller Big Monks mountain, both popular for walking and outdoor activities.
What is the geological makeup of the Banks suburb?
The surface geology is alluvium, while the surrounding hills consist of Deakin Volcanics, volcanic rocks formed about 414 million years ago during the Silurian period.