47 Olive Pink Crescent
47 Olive Pink Crescent, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jul 2010 | $652,500 | $787 |
| Sold | Dec 2003 | $212,000 | $255 |
| Sold | Sep 2002 | $159,500 | $192 |
Price per m² based on land size of 829 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714851040
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/114/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 829 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
How many bedrooms and bathrooms does the home have?
The home offers four bedrooms and two bathrooms, providing ample space for a family.
What is the size of the land the property sits on?
It sits on an 829 m² block, offering a sizable garden area.
What type of residence is located at 47 Olive Pink Crescent?
It is a detached house.
What parking facilities are available at the property?
The property includes two parking spaces for residents' vehicles.
What recreational parks are near the property?
Beau and Jessi Park is about 0.9 km away, Gordonvale Park is roughly 1.6 km distant, and the local Banks Oval is within 0.7 km, providing options for walking, picnics, and sports.
Are there any shopping facilities close to the home?
Yes, a small shopping centre on Pockett Avenue within the suburb offers take‑away food shops, a pet grooming shop, and a SUPAEXPRESS supermarket.
What natural reserves or features are near Banks?
To the east of Banks lies the Rob Roy Nature Reserve, part of Canberra Nature Park, which includes Mt Rob Roy, and the nearby Big Monks mountain offers a gliding stage for paragliders and hang‑gliders.
What is the geological composition of the area?
The surface geology of Banks is alluvium, while the surrounding hills consist of Deakin Volcanics formed during the Silurian age, about 414 million years ago.