28 Birrigai Square
28 Birrigai Square, Ngunnawal ACT 2913, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Sep 2017 | $405,000 | $1,100 |
| Sold | Oct 1993 | $113,446 | $308 |
| Sold | Jun 1993 | $43,000 | $116 |
Price per m² based on land size of 368 m².
Key details
- Locality
- Ngunnawal
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714898729
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/NGUN/20/20
- Remoteness area
- Metro
- Property type
- House
- Land size
- 368 m²
- Internal area
- 97 m²
- 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 is the land size of the house at 28 Birrigai Square?
The property sits on a 368 m² block. This provides a modestly sized yard for outdoor activities or gardening.
How many bedrooms and bathrooms does the home have?
The house offers two bedrooms and one bathroom, making it suitable for small families or couples.
Is there any on‑site parking available?
Yes, the property includes a single parking space for residents.
How far is the residence from major centres in Canberra?
It is located about 4 km from the Gungahlin Town Centre and roughly 13 km from Canberra’s central business district.
Which parks are within a short walk of the address?
Nearby green spaces include Homestead Park (approximately 0.3 km), Violets Park (around 0.5 km), Gold Creek Park (about 0.8 km), and Crinigan Park (also about 0.8 km).
What community facilities are close to 28 Birrigai Square?
The Arabanoo Street Library serves the neighbourhood, and the historic Gold Creek Homestead is a short distance away, offering cultural interest.
What geological features characterise the Ngunnawal area where the property is situated?
Ngunnawal sits on the Canberra Formation, primarily composed of slaty shale and mudstone, with outcrops of dacite, quartz‑andesite, and tuff. The terrain shows folding patterns aligned north‑north‑east with the Deakin Fault running near Ginninderra Creek.