21 Bokhara Circuit
21 Bokhara Circuit, Kaleen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2009 | $521,000 | $532 |
| Sold | Feb 2007 | $430,000 | $439 |
Price per m² based on land size of 979 m².
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714870419
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/50/17
- Remoteness area
- Metro
- Property type
- House
- Land size
- 979 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 21 Bokhara Circuit sits?
The property sits on a 979 m² block, offering ample space for a garden or outdoor activities.
How many bedrooms and bathrooms does the home have?
The house features three bedrooms and a single bathroom, suitable for a small family or downsizer.
What type of dwelling is 21 Bokhara Circuit?
It is a standalone house, providing private living accommodation on its own land.
What recreational facilities are available nearby?
Kaleen has several ovals, including Kaleen North, Enclosed, District Playing Fields, and South oval, supporting soccer, cricket, and rugby, plus a well‑maintained network of bicycle paths that run north‑south through the suburb.
Are there shopping options within walking distance?
The suburb includes two small shopping centres on Maribyrnong Avenue and a larger centre near Georgina Crescent; additionally, Kaleen Plaza is about 1–2 km away.
Which places of worship are close to the property?
Within roughly 1‑2 km are All Saints Greek Orthodox Church (≈1.2 km) and other local churches such as the Anglican St Simon’s and St Mark Coptic Orthodox, providing a range of worship options.
What geological features are characteristic of the Kaleen area?
The eastern part of Kaleen sits on Silurian‑age calcareous shale, while the western side is underlain by Ordovician greywacke, separated by the Gungahlin Fault; the Winslade Fault also runs nearby to the east.