23 Mortlock Circuit
23 Mortlock Circuit, Kaleen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2009 | $761,000 | $1,010 |
| Sold | Mar 2007 | $533,000 | $707 |
Price per m² based on land size of 753 m².
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714868255
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/143/12
- Remoteness area
- Metro
- Property type
- House
- Land size
- 753 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 house at 23 Mortlock Circuit have?
The property features four bedrooms and three bathrooms. All rooms are part of a single‑storey family home.
What is the size of the land parcel for this house?
The house sits on a 753 m² block, offering ample space for outdoor living and landscaping.
Where exactly is 23 Mortlock Circuit located within Kaleen?
It is situated on Mortlock Circuit in the suburb of Kaleen, part of Canberra’s Belconnen district and bordered by Baldwin Drive and Ginninderra Drive.
What recreational facilities are nearby?
Kaleen hosts several ovals, including Kaleen North, Enclosed, District Playing Fields and South, within a short drive, and Fern Hill Park is about 1‑2 km away. The suburb also has well‑maintained bicycle paths that run north‑south through the area.
How far is the nearest shopping centre?
Kaleen Plaza, the local shopping centre, is approximately 1‑2 km from the property.
Are there any natural landmarks close to the house?
Reservoir Hill lies just 0.4 km to the west, and the Lyneham Ridge eucalypt plantation borders the eastern side of Kaleen, offering nearby natural scenery.
What is notable about the geology of Kaleen?
The suburb sits on Silurian‑age Canberra Formation calcareous shale to the east and Ordovician‑age Pittman Formation greywacke to the west, separated by the Gungahlin Fault.