9A Conner Close
9A Conner Close, Palmerston ACT 2913, Australia
Key details
- Locality
- Palmerston
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714905497
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/PALM/159/7/7
- Remoteness area
- Metro
- Property type
- Unit
- Land size
- 2584 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 residence is 9A Conner Close?
9A Conner Close is a unit located in the suburb of Palmerston, within the Gungahlin district of Canberra. It offers a low‑rise, multifamily living option.
How many bedrooms and bathrooms does the unit have?
The unit features three bedrooms and two bathrooms, providing accommodation suitable for families or shared living arrangements.
What is the size of the land associated with the property?
The property sits on a land parcel of approximately 2,584 m², giving it a generous outdoor footprint relative to typical urban units.
Which public transport services are accessible from the property?
ACTION bus routes 21, 22, 23 and 24 travel along nearby Kosciuszko Avenue, connecting the area to Gungahlin Town Centre, Franklin and Nicholls. The Gungahlin Place light‑rail stop is also about 1‑2 km away.
What recreational amenities are close to 9A Conner Close?
Within a kilometre you’ll find the Gungahlin Enclosed Oval, Gungahlin United Football Club facilities, and parks such as Ginninderra Park, Girrawah Park and George Kemp Park for outdoor activities.
Where is Palmerston located within Canberra?
Palmerston is a residential suburb in the Gungahlin district of Canberra, bordered by Gungahlin Drive and Gundaroo Drive and adjacent to Nicholls, Gungahlin, Crace and Franklin.
What geological characteristics define the Palmerston area?
The suburb sits on the late middle Silurian Canberra Formation, primarily composed of slaty shale and mudstone with notable ashstone exposures shaped by anticlines, synclines and local faults such as the Winslade and Gungahlin faults.