16 Goessling Place
Flynn ACT 2615, Australia
Key details
- Locality
- Flynn
- State
- ACT
- Coordinates
Latitude and longitude for the mapped property location.
- 35.20515013 / 149.04686254
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714866547
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/FLYN/17/29
- Remoteness area
- Metro
- Property type
- House
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sale | 14 Dec 2024 | $761,000 | — |
Real Estate Agencies
Nearby schools
Frequently asked questions
How many bedrooms and bathrooms are in the home at 16 Goessling Place?
The property offers four bedrooms and a single bathroom. It provides ample space for a family
What parking options are available at this address?
The house includes four parking spaces for residents and guests. No garage is mentioned in the listing
Where is 16 Goessling Place situated within Canberra?
It is located in the suburb of Flynn, part of the Belconnen district of Canberra, ACT. Flynn lies between Tillyard Drive, Kingsford Smith Drive and Ginninderra Drive
How close is the property to local parks?
George Simpson Park is positioned about 0.5 km from the home, making it a convenient walking distance. The Boslem and Harte Park is also nearby, roughly 1.2 km away
Which neighbouring suburbs surround this property?
The residence is adjacent to the suburbs of Charnwood, Fraser, Melba, Latham and Spence. These areas are all within a short drive or walk
What electoral divisions cover the Flynn area?
Federally, Flynn falls within the Division of Fenner. For ACT Legislative Assembly elections, it is part of the Ginninderra electorate
What geological features are characteristic of the Flynn suburb?
The south‑west of Flynn sits on Deakin Volcanics purple rhyodacite, while the north‑east contains Hawkins Volcanics green‑grey dacite and quartz‑andesite. These two formations are separated by the Deakin Fault
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