53 Barber Crescent
53 Barber Crescent, Flynn ACT 2615, Australia
Key details
- Locality
- Flynn
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714874087
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/FLYN/9/6
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1418 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 53 Barber Crescent, Flynn?
It is a standalone house situated in the suburb of Flynn. The home offers a family‑oriented layout typical of the area.
How many bedrooms does the property have?
The house features five bedrooms, providing ample space for a larger household or flexible living arrangements.
What is the size of the land on which the house sits?
The property sits on a 1,418 m² block, offering a generous yard area for outdoor activities, gardening, or future extensions.
Which major roads provide access to Flynn and the property?
Flynn is bordered by Tillyard Drive, Kingsford Smith Drive and Ginninderra Drive, giving convenient connectivity to surrounding suburbs and the Canberra centre.
What parks or natural landmarks are located near 53 Barber Crescent?
George Simpson Park is about 1–2 km away, and The Boslem and Harte Park is roughly 1–2 km distant. The nearby Mount Rogers hill lies within 1 km, offering a scenic natural backdrop.
Why is the suburb named Flynn?
Flynn is named after John Flynn, a Presbyterian minister who founded the Australian Inland Mission Aerial Medical service in 1928, the precursor to the Royal Flying Doctor Service. The suburb name was officially gazetted on 9 September 1971.
What geological features are common in the Flynn area?
The southwest part of Flynn is dominated by Deakin Volcanics purple rhyodacite, while the north contains Hawkins Volcanics with green‑grey dacite and quartz andesite. The Deakin Fault separates these volcanic units, and a band of Glebe Farm Adamellite intrudes the region.