41 Olive Pink Crescent
41 Olive Pink Crescent, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jul 2010 | $630,000 | $893 |
| Sold | Mar 2005 | $180,000 | $255 |
| Sold | Sep 2002 | $149,500 | $212 |
Price per m² based on land size of 705 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714851043
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/114/4
- Remoteness area
- Metro
- Property type
- House
- Land size
- 705 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 are in the home at 41 Olive Pink Crescent?
The property offers three bedrooms and two bathrooms, providing space for a small family or guests.
What is the size of the land and how many parking spaces does the house have?
It sits on a 705 m² block and includes two parking spaces for vehicles.
Which parks or recreational areas are closest to the property?
Beau and Jessi Park is about 0.9 km away, Gordonvale Park is roughly 1.6 km distant, and the suburb’s own Banks Oval is within the local area for community events.
Is there a grocery store nearby?
A small shopping centre on Pockett Avenue within Banks contains a SUPAEXPRESS supermarket, making daily shopping convenient.
Why is the suburb called Banks?
Banks is named after Sir Joseph Banks, the botanist who sailed with Captain James Cook to Botany Bay in 1770.
What natural attractions lie to the east of Banks?
The Rob Roy Nature Reserve, part of Canberra Nature Park, is directly east and includes Mount Rob Roy, while the smaller mountain Big Monks, popular with paragliders, is also nearby.
What is the underlying geology of the Banks area?
The surface of the suburb is covered by alluvium, and beneath it the hills are composed of Deakin Volcanics that erupted during the Silurian period about 414 million years ago.