34 Tyrrell Circuit
34 Tyrrell Circuit, Kaleen ACT 2617, Australia
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714874101
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/60/13
- Remoteness area
- Metro
- Property type
- House
- Land size
- 987 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 type of property is located at 34 Tyrrell Circuit?
34 Tyrrell Circuit is a detached house situated on a 987 m² block of land. The residence benefits from a sizable garden area within the Kaleen suburb.
What recreational facilities are nearby for sports and outdoor activities?
Kaleen hosts several ovals, including Kaleen North oval, Kaleen Enclosed oval, Kaleen District Playing Fields, and Kaleen South oval, where soccer, cricket and rugby are played. The suburb also features well‑maintained bicycle paths that run north‑south through the area.
Where can I find shopping amenities close to the property?
A small shopping centre on Maribyrnong Avenue borders the main street and is within walking distance. Additionally, Kaleen Plaza is located about 0.5 km away, offering further retail options.
Which places of worship are located near 34 Tyrrell Circuit?
All Saints Greek Orthodox Church is approximately 0.3 km from the property. Nearby also stand St Mark Coptic Orthodox Church and St Simon’s Anglican Church on Georgina Crescent.
What major roads and transport routes serve the Kaleen suburb?
Kaleen is bordered by Baldwin Drive and Ginninderra Drive, providing easy road access. The 2XX transmitting station near the Barton Highway also indicates proximity to a major arterial route.
What geological features are characteristic of the Kaleen area?
The eastern part of Kaleen sits on Silurian‑age calcareous shale of the Canberra Formation, while the western side rests on Ordovician greywacke of the Pittman Formation. These two sediment types are separated by the Gungahlin Fault.