2 Castor Place
2 Castor Place, Giralang ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Feb 2000 | $225,000 | $256 |
| Sold | Jul 1991 | $198,155 | $226 |
Price per m² based on land size of 876 m².
Key details
- Locality
- Giralang
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714866515
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/GIRA/95/2
- Remoteness area
- Metro
- Property type
- House
- Land size
- 876 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 is the land size of the property at 2 Castor Place?
The property sits on a block of 876 m². This provides ample space for a garden, outdoor activities, or future extensions.
What type of dwelling is located at 2 Castor Place?
2 Castor Place is a standalone house. It offers private living accommodation within the Giralang suburb.
What does the name “Giralang” mean and how was it chosen?
Giralang is derived from a Wiradhuri word meaning “star.” The suburb’s name reflects a theme of Aboriginal words for stars, astronomers and constellations.
Which recreational or community facilities are close to the property?
Belconnen United FC, a local football club, is about 0.5 km away, and the Kaleen Plaza shopping centre is roughly 1.3 km distant, offering shops and services. The All Saints Greek Orthodox Church in Kaleen is also nearby at around 1.4 km.
Are there any heritage or natural sites near 2 Castor Place?
Yes, the Synemon Plana moth habitat, a natural Commonwealth heritage site, is approximately 0.6 km away. The historic Royal Australian Naval Transmitting Station is also close, at about 1 km distance.
What are the main geological features of the Giralang area?
Giralang sits on a mix of Ordovician Pittman Formation greywacke and turbidites, with Acton Shale on its eastern edge. Further inland, late Silurian sedimentary rocks such as mudstone, State Circle Shale, and micaceous Black Mountain Sandstone are common, and a north‑west‑trending fault aligns with Ginninderra Creek.