10 Bingle Street
10 Bingle Street, Flynn ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Oct 2019 | $655,000 | $849 |
| Sold | Aug 1999 | $142,000 | $184 |
| Sold | Oct 1994 | $164,000 | $212 |
Price per m² based on land size of 771 m².
Key details
- Locality
- Flynn
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714862106
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/FLYN/17/20
- Remoteness area
- Metro
- Property type
- House
- Land size
- 771 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 10 Bingle Street?
It is a standalone house featuring four bedrooms and two bathrooms. The property also includes two parking spaces and sits on a 771 m² block of land.
How large is the land parcel for this house?
The land area measures 771 square metres, providing ample space for a garden or outdoor activities.
What parking facilities are available at the property?
The home provides two dedicated parking spaces for residents and guests.
Which parks are close to 10 Bingle Street?
George Simpson Park is just 0.4 km away, and The Boslem And Harte Park is about 1.2 km from the property, both offering green space and recreation.
What surrounding suburbs are nearest to this address?
Flynn itself is 0.4 km away, with Melba 0.7 km, Charnwood 1.1 km, and Spence approximately 1.8 km from the location.
Which electoral districts does the property fall under?
Federally, it is part of the Division of Fenner, while for ACT Legislative Assembly elections it lies in the Ginninderra electorate.
What is the geological makeup of the area around Flynn?
The southwest of Flynn is dominated by Deakin Volcanics purple rhyodacite, with grey rhyodacitic tuff and green‑grey rhyodacite to the south. The Deakin Fault separates these from the Hawkins Volcanics, which consist of green‑grey dacite and quartz‑andesite in the north.