9 Buller Crescent
9 Buller Crescent, Palmerston ACT 2913, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jul 2001 | $171,000 | $206 |
| Sold | Jul 1992 | $55,500 | $67 |
Price per m² based on land size of 827 m².
Key details
- Locality
- Palmerston
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714909702
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/PALM/122/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 827 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 located at 9 Buller Crescent?
The property at 9 Buller Crescent is a detached house. It sits on its own block within the Palmerston suburb.
How large is the land parcel for this house?
The house sits on an 827 m² land parcel. This provides ample space for a garden or outdoor entertaining area.
Which public transport options are available nearby?
ACTION bus routes 21 and 22 travel along Kosciuszko Avenue, while routes 23 and 24 run through half of Palmerston, linking the area to Gungahlin Town Centre, Franklin and Nicholls.
How far is the nearest light‑rail stop from the property?
Gungahlin Place, the closest light‑rail station, is about 1.5 km away, providing easy access to the wider Canberra rail network.
What recreational facilities are within walking distance?
Nearby amenities include Gungahlin Enclosed Oval (≈0.9 km), Ginninderra Park (≈0.9 km), Girrawah Park (≈1.2 km) and the Gungahlin United Football Club facilities (≈0.9 km).
What shopping options are close to 9 Buller Crescent?
Marketplace Gungahlin, a regional shopping centre, is roughly 1.4 km away, offering a range of retail and dining options.
What is the geological makeup of the area surrounding the property?
Palmerston sits on the Canberra Formation from the late middle Silurian age, primarily composed of slaty shale and mudstone. Visible ashstone exposures form a 75‑metre‑wide ear‑of‑corn shape, with nearby faults such as the Winslade and Gungahlin faults influencing the local geology.