6 Wyola Place
6 Wyola Place, Kaleen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2024 | Unknown | — |
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714878105
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/20/9
- Remoteness area
- Metro
- Property type
- House
- 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 6 Wyola Place have?
The property includes three bedrooms and two bathrooms. It is a standalone house.
What shopping options are available near 6 Wyola Place?
Kaleen Plaza is just about 0.7 km away, offering a range of retail services. The suburb also has two smaller shopping centres on Maribyrnong Avenue and a larger centre near the border with Giralang on Georgina Crescent.
Are there any places of worship close to the property?
Yes, All Saints Greek Orthodox Church is approximately 0.8 km from the home. Other nearby churches include St. Simon's Anglican Church and St. Mark Coptic Orthodox Church, both located near Georgina Crescent.
What sports and recreation facilities are near 6 Wyola Place?
Kaleen features several ovals, North, Enclosed, District Playing Fields, and South, that host soccer, cricket and rugby. George Kemp Park is also about 1.3 km away, providing open green space.
How is cycling infrastructure in Kaleen for residents of 6 Wyola Place?
Kaleen is traversed by a well‑maintained bicycle network, with the main north‑south track passing under Ginninderra Drive and running through the suburb. This makes it easy for cyclists to travel locally and into neighbouring areas.
What is the geological composition of the area surrounding the property?
The eastern part of Kaleen sits on Silurian‑age Canberra Formation calcareous shale, while the western side rests on Ordovician‑age Pittman Formation greywacke. These two formations are separated by the Gungahlin Fault, with the Winslade Fault also present to the east.