44 Olive Pink Crescent
44 Olive Pink Crescent, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2017 | $680,000 | $1,100 |
| Sold | May 2006 | $492,500 | $796 |
Price per m² based on land size of 618 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714854258
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/115/22
- Remoteness area
- Metro
- Property type
- House
- Land size
- 618 m²
- Internal area
- 291 m²
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Real Estate Agencies
Nearby schools
Frequently asked questions
How many bedrooms and bathrooms does the house at 44 Olive Pink Crescent have?
The property features four bedrooms and two bathrooms, providing ample space for a family or guests.
What is the size of the land that the house occupies?
The house sits on a 618 m² block, offering a generous outdoor area for gardening, entertaining or future extensions.
How many parking spaces are available for residents?
There are two dedicated parking spaces supplied with the property.
Which parks are located near 44 Olive Pink Crescent and how far away are they?
Beau and Jessi Park is about 0.7 km away, while Gordonvale Park is roughly 1.6 km from the home, both providing easy access to green space.
Is there a shopping centre within walking distance of the property?
Yes, a small local shopping centre on Pockett Avenue lies within the suburb, offering a supermarket, take‑away food shops and a pet grooming service.
What natural reserves or landmarks are close to the property?
To the east of Banks are the Rob Roy Nature Reserve and the smaller Big Monks mountain, popular with hikers and paragliders.
What is the geological makeup of the area surrounding 44 Olive Pink Crescent?
The surface geology of Banks is alluvium, underlain by Deakin Volcanics that formed during the Silurian age around 414 million years ago.