60 Diamantina Crescent
60 Diamantina Crescent, Kaleen ACT 2617, Australia
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714869663
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/112/20
- Remoteness area
- Metro
- Property type
- House
- Land size
- 687 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
What is the size of the land this house occupies?
The property sits on a 687 m² block. It provides ample garden space within the Kaleen neighbourhood.
How close are local shopping facilities to the house?
Kaleen Plaza, a small shopping centre, is just about 0.8 km away, and there are two additional shopping strips on Maribyrnong Avenue nearby, offering convenient access to everyday retail.
What recreational areas are available nearby?
The suburb features several ovals, including Kaleen North and South ovals, and the Kaleen District Playing Fields, while Fern Hill Park is roughly 1.8 km away, providing ample space for sports and leisure.
Are there any places of worship close to the property?
All Saints Greek Orthodox Church is only 0.7 km from the house, and other nearby churches include St Mark Coptic Orthodox Church and St Simon’s Anglican Church, all within walking distance.
Which major roads provide access to the property?
The suburb is bordered by Baldwin Drive and Ginninderra Drive, offering direct routes to the Barton Highway and other parts of Canberra.
Is there bicycle infrastructure in Kaleen?
Kaleen is criss‑crossed by well‑maintained bicycle paths, including a main north‑south track that passes under Ginninderra Drive, making the area very bike‑friendly.
What can you tell me about the geology of the area?
The eastern part of Kaleen sits on Silurian‑age Canberra Formation calcareous shale, while the western side rests on Ordovician‑age Pittman Formation greywacke, separated by the Gungahlin Fault.