13 Inlander Crescent
13 Inlander Crescent, Flynn ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 2008 | $437,500 | $401 |
| Sold | Jul 1999 | $172,500 | $158 |
Price per m² based on land size of 1090 m².
Key details
- Locality
- Flynn
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714869702
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/FLYN/28/20
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1090 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
How many bedrooms and bathrooms are in the house at 13 Inlander Crescent?
The property features four bedrooms and four bathrooms. All rooms are part of a single‑storey house.
What is the size of the land parcel for this residence?
The house sits on a 1,090 m² block, providing ample space for outdoor activities and landscaping.
How many parking spaces does the property provide?
There are four parking spaces available on the premises, conveniently located for residents and guests.
Where is 13 Inlander Crescent situated within the suburb of Flynn?
It is located in Flynn, a suburb of the Belconnen district in Canberra, positioned between Tillyard Drive, Kingsford Smith Drive and Ginninderra Drive. The surrounding suburbs include Charnwood, Fraser, Melba, Latham and Spence.
What parks are located close to this address?
George Simpson Park is approximately 0.5 km away, and The Boslem and Harte Park lies about 1.5 km from the property, offering nearby green space for recreation.
What are the notable geological features of the Flynn area?
The southwest part of Flynn is dominated by Deakin Volcanics purple rhyodacite, with grey rhyodacitic tuff and green‑grey rhyodacite present as well. The Deakin Fault separates these rocks from the Hawkins Volcanics to the north‑east, which include green‑grey dacite and quartz‑andesite.