52 Jacka Crescent
52 Jacka Crescent, Campbell ACT 2612, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 1994 | $335,000 | $236 |
Price per m² based on land size of 1416 m².
Key details
- Locality
- Campbell
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714883925
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/CAMP/16/16
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1416 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 property is located at 52 Jacka Crescent?
It is a house situated in the suburb of Campbell, Australian Capital Territory. The property benefits from being set within a residential neighbourhood that borders Mount Ainslie.
How much land does the property sit on?
The house sits on a 1,416 m² parcel of land, providing ample space for outdoor activities or potential landscaping.
What parks or green spaces are close to the property?
Legacy Park is just 0.2 km away, while RSL Park and George Cross Park are each within about 0.3‑0.5 km. These parks offer mature native trees, open lawns, and playground facilities.
Which notable national institutions are near the property?
The Australian War Memorial, the Royal Military College Duntroon, and the Australian Defence Force Academy are all located in Campbell, making cultural and historical attractions easily reachable.
What is the historical significance of the suburb of Campbell?
Campbell is named after Robert Campbell, owner of the historic Duntroon station. Many buildings associated with his family, such as Duntroon House and Yarralumla House, remain prominent landmarks in the area.
What geological features underlie the area around 52 Jacka Crescent?
The suburb sits on the lowest layer of the Ainslie Volcanics, comprising grey dacite, agglomerate and tuff formed in the Silurian period. Additional layers of grey quartz andesite and cream rhyolite are present to the north and north‑east.