41 Gellibrand Street
41 Gellibrand Street, Campbell ACT 2612, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2021 | $1,730,000 | $1,803 |
| Sold | Jan 2010 | $878,000 | $915 |
| Sold | Apr 1992 | $212,000 | $221 |
Price per m² based on land size of 959 m².
Key details
- Locality
- Campbell
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714888018
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/CAMP/58/9
- Remoteness area
- Metro
- Property type
- House
- Land size
- 959 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 size of the land that the house sits on?
The property occupies a land parcel of 959 m². This provides a generous outdoor area for gardening or recreation.
How many bedrooms and bathrooms does the home have?
The house features four bedrooms and one bathroom, offering ample space for a growing family or guests.
Is any parking provided with the property?
Yes, the property includes one designated parking space for a vehicle.
What major educational institutions are located nearby?
The Australian Defence Force Academy is about 0.4 km away, and the UNSW Canberra campus is roughly 0.5 km from the house, making them within easy walking distance.
Which parks or recreational areas are close to the home?
Victoria Cross Park is approximately 0.8 km away and Legacy Park is about 1 km distant, offering green space and walking trails nearby.
Are there any historic heritage sites in the vicinity?
Several heritage sites are within about 1 km, including the General Bridges Grave, Captains Quarters Assets B1‑B4, and the RMC Duntroon Conservation Area.
What is the underlying geology of the Campbell area?
Campbell sits on the lower layer of the Ainslie Volcanics, consisting mainly of grey dacite with agglomerate and tuff, formed during the Silurian period.