65 Waller Crescent
65 Waller Crescent, Campbell ACT 2612, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2001 | $339,000 | $375 |
| Sold | Apr 1997 | $206,000 | $228 |
| Sold | Jun 1994 | $212,000 | $234 |
| Sold | Mar 1993 | $189,950 | $210 |
| Sold | Jun 1991 | $165,000 | $182 |
Price per m² based on land size of 903 m².
Key details
- Locality
- Campbell
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714884853
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/CAMP/26/3
- Remoteness area
- Metro
- Property type
- House
- Land size
- 903 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 does the house at 65 Waller Crescent have?
The property features four bedrooms. It provides ample space for a medium-sized family.
What is the size of the land on which 65 Waller Crescent is built?
The house sits on a 903 m² block. This generous lot offers room for a garden or outdoor entertaining area.
What type of dwelling is located at 65 Waller Crescent?
65 Waller Crescent is a standalone house. It is a detached residential property within the Campbell suburb.
How far is the property from Victoria Cross Park?
Victoria Cross Park is about 0.2 km away, roughly a two‑minute walk. The park provides nearby green space for recreation.
Which notable landmarks are located within 1 km of 65 Waller Crescent?
Within roughly 1 km you will find the Australian War Memorial (≈0.9 km), George Cross Park (≈0.7 km), Remembrance Nature Park (≈0.8 km) and the Kemal Atatürk Memorial (≈0.9 km). These sites offer cultural and outdoor attractions close to the home.
What geological features characterize the area around 65 Waller Crescent?
Campbell sits on the lowest layer of the Ainslie Volcanics, a grey dacite with agglomerate and tuff. To the north the geology shifts to grey quartz andesite, and the north‑east features cream rhyolite from the upper volcanic layers.