54 Diamantina Crescent
54 Diamantina Crescent, Kaleen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 2008 | $380,000 | $322 |
Price per m² based on land size of 1178 m².
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714870763
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/112/17
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1178 m²
- Internal area
- -
- 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 home at 54 Diamantina Crescent have?
The property includes three bedrooms and two bathrooms.
What is the land size of the property at 54 Diamantina Crescent?
The house is situated on a block of approximately 1,178 m².
What recreational facilities are available nearby in Kaleen?
Kaleen features several ovals, including Kaleen North, Enclosed, District Playing Fields and South, supporting sports such as soccer, cricket and rugby, and a well‑maintained network of bicycle paths that run north‑south through the suburb.
What shopping options are close to 54 Diamantina Crescent?
The property is about 0.8 km from Kaleen Plaza, a local shopping centre, and there are two smaller shopping centres on Maribyrnong Avenue nearby.
Which major roads and bike routes serve the area around 54 Diamantina Crescent?
Kaleen is bordered by Baldwin Drive and Ginninderra Drive, providing easy road access, while the main bike track passes under Ginninderra Drive and runs north‑south through the suburb.
How did the suburb of Kaleen get its name?
The name Kaleen comes from the Wiradjuri word for “water,” reflecting the Aboriginal linguistic heritage of the area.
What geological formations underlie Kaleen?
The eastern side of Kaleen sits on Silurian‑age Canberra Formation calcareous shale, whereas the western side rests on Ordovician‑age Pittman Formation greywacke, separated by the Gungahlin Fault.