3 Campaspe Circuit
3 Campaspe Circuit, Kaleen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 2008 | $140,000 | $167 |
Price per m² based on land size of 837 m².
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714871663
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/55/9
- Remoteness area
- Metro
- Property type
- House
- Land size
- 837 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 3 Campaspe Circuit sits?
The property sits on a block of approximately 837 m². This provides ample space for outdoor activities and potential landscaping.
How many bedrooms and bathrooms does the home have?
The house features three bedrooms and one bathroom, making it suitable for a small family or those looking for extra room.
What type of dwelling is located at 3 Campaspe Circuit?
It is a standalone house, offering private living space within the Kaleen suburb.
What recreational facilities are nearby in Kaleen?
Kaleen hosts several ovals, including Kaleen North, Enclosed, District Playing Fields, and South, where soccer, cricket and rugby are played. The suburb also has well‑maintained bicycle paths that run north‑south through the area.
How close is the nearest shopping centre to the property?
Kaleen Plaza, a local shopping centre, is about 1.1 km away, providing convenient access to shops and services.
Are there any places of worship within walking distance of the home?
Yes, All Saints Greek Orthodox Church is roughly 1 km away, and other nearby churches include a Coptic Orthodox church and St. Simon's Anglican church on Georgina Crescent.
What is notable about the geology of Kaleen?
The eastern part of Kaleen sits on Silurian‑age calcareous shale, while the west contains Ordovician greywacke. These two formations are separated by the Gungahlin Fault, which has uplifted the older greywacke.