163 Chuculba Crescent
163 Chuculba Crescent, Giralang ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 2004 | $433,000 | $480 |
| Sold | Feb 2002 | $259,000 | $287 |
Price per m² based on land size of 901 m².
Key details
- Locality
- Giralang
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714866348
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/GIRA/68/2
- Remoteness area
- Metro
- Property type
- House
- Land size
- 901 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 dwelling is located at 163 Chuculba Crescent?
It is a standalone house featuring four bedrooms and two bathrooms.
How large is the land that the property sits on?
The property sits on a 901 m² block of land.
What does the name ‘Giralang’ mean?
Giralang comes from a Wiradhuri word meaning “star,” reflecting the suburb’s theme of Aboriginal astronomical names.
Which shopping and community facilities are close to the address?
Kaleen Plaza shopping centre is about 0.6 km away, and the All Saints Greek Orthodox church in Kaleen is roughly 0.8 km from the home.
What natural or recreational sites are within a couple of kilometres?
George Kemp Park (≈1.4 km) and Gungahlin Hill (≈1.3 km) provide nearby green space and walking opportunities.
Are there any heritage or environmental sites near the property?
The Royal Australian Naval Transmitting Station (≈1.1 km) and the Synemon Plana moth habitat (≈1.2 km) are recognized heritage and natural sites in the vicinity.
What geological features characterize the Giralang area?
The suburb sits on Ordovician Pittman Formation greywacke and turbidites, with bands of Acton Shale, late Silurian sedimentary rocks, mudstone, State Circle Shale, micaceous Black Mountain Sandstone, and calcareous shale from the Canberra Formation, intersected by a north‑west‑trending fault.