20 Canopus Crescent
20 Canopus Crescent, Giralang ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Built | Unknown | — |
Price per m² based on land size of 898 m².
Key details
- Locality
- Giralang
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714864090
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/GIRA/20/7
- Remoteness area
- Metro
- Property type
- House
- Land size
- 898 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
How many bedrooms and bathrooms does the house have?
The property features four bedrooms and one bathroom. It is a standalone house suitable for families seeking spacious living.
What is the size of the land the house sits on?
The home occupies a generous 898 m² block, providing ample outdoor space for gardens, recreation, or potential extensions.
How far is the property from the nearest shopping centre?
Kaleen Plaza, a local shopping centre with retail and dining options, is about 1.4 km away, a short drive or cycle ride from the house.
What natural or heritage sites are close to the property?
Within roughly 1 km you’ll find the Synemon Plana Moth Habitat, a Commonwealth heritage site, and about 1.4 km away the historic Royal Australian Naval Transmitting Station, both offering unique local interest.
What does the name ‘Giralang’ mean?
Giralang comes from a Wiradhuri word meaning “star.” The suburb’s streets are also named after Aboriginal words for stars, astronomers and southern‑hemisphere constellations.
Are there any recreational facilities nearby?
The Giralang District Playing fields are located within the suburb, providing open space for sports and community activities close to the residence.
What geological features characterize the Giralang area?
Giralang sits on varied geology, including Ordovician Pittman Formation greywacke, Silurian sedimentary rocks such as State Circle Shale and Black Mountain Sandstone, and a north‑west trending fault marked by an iron‑oxide reef.