10 Biala Place
10 Biala Place, Ngunnawal ACT 2913, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2002 | $254,000 | $340 |
| Sold | Nov 1997 | $41,000 | $55 |
| Sold | Mar 1997 | $40,000 | $53 |
Price per m² based on land size of 745 m².
Key details
- Locality
- Ngunnawal
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714904891
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/NGUN/64/23
- Remoteness area
- Metro
- Property type
- House
- Land size
- 745 m²
- Internal area
- 149 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
How many bedrooms and bathrooms does the house at 10 Biala Place have?
The house features four bedrooms and two bathrooms, providing ample space for a growing family or guests.
What is the land size of the property?
The property sits on a 745 m² block, giving room for outdoor activities and potential landscaping.
What parking facilities are included with the house?
The home includes a garage that accommodates two parking spaces.
How far is the property from the Gungahlin Town Centre and the centre of Canberra?
Ngunnawal is approximately 4 km from the Gungahlin Town Centre and about 13 km from the centre of Canberra, making both easily reachable by car.
Which parks are located within walking distance of the property?
Nearby parks include Gold Creek Park (about 0.2 km away), Homestead Park (0.5 km), Violets Park (around 1 km), Girrawah Park (≈1.4 km), Crinigan Park (≈1.5 km) and Ginninderra Park (≈1.9 km).
What heritage or community attractions are close to the house?
Gold Creek Homestead, a historic attraction, is situated roughly 0.6 km from the property, offering cultural and recreational interest.
What is the geological makeup of the Ngunnawal area where the property is located?
Ngunnawal sits on the Canberra Formation, mainly composed of slaty shale and mudstone, with dacite and quartz‑andesite outcrops in the north‑west corner, tuff and ashstone exposures, and folded rock structures aligned north‑northeast. The Deakin Fault runs near the eastern side along Ginninderra Creek.