12 Betty Maloney Crescent
12 Betty Maloney Crescent, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 2021 | $802,000 | $1,782 |
| Sold | Aug 2013 | $458,000 | $1,017 |
| Sold | Sep 2004 | $328,000 | $728 |
Price per m² based on land size of 450 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714852200
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/36/34
- Remoteness area
- Metro
- Property type
- House
- Land size
- 450 m²
- Internal area
- 121 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
How many bedrooms and bathrooms does the house at 12 Betty Maloney Crescent have?
The property features three bedrooms and two bathrooms, providing ample space for a small family or shared living arrangements.
What is the land size of the property?
The house sits on a 450 m² block, offering a modest outdoor area within the suburb of Banks.
What type of dwelling is located at 12 Betty Maloney Crescent?
It is a separate house, distinguishing it from townhouses or apartments in the area.
What recreational facilities are close to the address?
Beau and Jessi Park is just about 0.2 km away, and Banks Oval is within the suburb, both popular for community sports and outdoor activities.
Is there a shopping centre nearby?
Yes, a small shopping centre on Pockett Avenue, featuring two take‑away food shops, a pet grooming outlet and a SUPAEXPRESS supermarket, is located within the suburb.
What natural reserves are situated near Banks?
The Rob Roy Nature Reserve, part of Canberra Nature Park, lies to the east of Banks and includes the hilly terrain of Mt Rob Roy, while the smaller mountain Big Monks is also nearby and offers a gliding stage for paragliders.
What geological features underlie the suburb of Banks?
The surface geology is alluvium, and beneath it the hills are composed of the Silurian‑age Deakin Volcanics, which erupted around 414 million years ago.