58 Mortlock Circuit
58 Mortlock Circuit, Kaleen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 1993 | $88,400 | $109 |
| Sold | Mar 1991 | $143,000 | $176 |
Price per m² based on land size of 811 m².
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714866819
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/144/12
- Remoteness area
- Metro
- Property type
- House
- Land size
- 811 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 on which the house at 58 Mortlock Circuit sits?
The property sits on a land parcel of 811 m². This provides a modest block size for a detached house in Kaleen.
What type of dwelling is located at 58 Mortlock Circuit?
58 Mortlock Circuit is a standalone house. It is one of the residential homes within the Kaleen suburb.
How far is the property from the University of Canberra?
The University of Canberra is about 1 km away from the house, making it a short walk or bike ride to the campus.
What shopping facilities are near 58 Mortlock Circuit?
Kaleen has two small shopping centres on Maribyrnong Avenue and a larger centre near Georgina Crescent. Kaleen Plaza is also roughly 1.5 km from the property.
Are there any parks or recreational areas close to the house?
Yes, Fern Hill Park is approximately 1.2 km away, and Kaleen features several ovals such as Kaleen North Oval and Kaleen District Playing Fields for sports like soccer, cricket and rugby.
Does Kaleen have bicycle infrastructure near the property?
Kaleen is served by a well‑maintained network of bicycle paths. The main track runs north–south through the suburb and passes under Ginninderra Drive.
What geological features are characteristic of Kaleen?
The suburb sits on Silurian‑age Canberra Formation calcareous shale in the east and Ordovician‑age Pittman Formation greywacke in the west. The Gungahlin Fault separates these sediments, with the Winslade Fault also present to the east.