11 Amagula Avenue
11 Amagula Avenue, Ngunnawal ACT 2913, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Apr 1994 | $169,680 | $275 |
| Sold | Nov 1993 | $62,100 | $100 |
Price per m² based on land size of 615 m².
Key details
- Locality
- Ngunnawal
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714902273
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/NGUN/28/7
- Remoteness area
- Metro
- Property type
- House
- Land size
- 615 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 11 Amagula Avenue?
The address is a standalone house situated in the suburb of Ngunnawal, ACT. It forms part of the primarily residential character of the area.
How large is the land parcel for the house at 11 Amagula Avenue?
The property sits on a 615 m² block. This size provides space for a garden or outdoor activities typical of suburban homes.
How far is the property from the Gungahlin Town Centre?
Ngunnawal is located approximately 4 km from the Gungahlin Town Centre. The distance makes it convenient to access shopping, dining and transport services.
Which parks are within walking distance of 11 Amagula Avenue?
Girrawah Park is about 0.2 km away, Ginninderra Park sits roughly 0.5 km from the house, and Violets Park is around 0.6 km distant. All three parks are easily reachable on foot.
What community facilities are nearby the property?
The Arabanoo Street Library serves local residents, and New Life Presbyterian Church is located on nearby Wanganeen Avenue. The historic Gold Creek Homestead, a local attraction, is also just about 1 km away.
What is notable about the geology of the Ngunnawal area where the property sits?
Ngunnawal rests on the Canberra Formation, predominantly composed of slaty shale and mudstone, with areas of dacite, quartz‑andesite, and tuff exposures. The rock structures show north‑north‑east folds and the Deakin Fault runs parallel to the folds along Ginninderra Creek.