17 Jacka Crescent
17 Jacka Crescent, Campbell ACT 2612, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Sep 2019 | $990,000 | $1,506 |
| Sold | Jul 1998 | $215,000 | $327 |
| Sold | Feb 1997 | $197,000 | $299 |
| Sold | May 1990 | $143,000 | $217 |
Price per m² based on land size of 657 m².
Key details
- Locality
- Campbell
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714884054
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/CAMP/12/33
- Remoteness area
- Metro
- Property type
- House
- Land size
- 657 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 and internal layout of 17 Jacka Crescent?
The property sits on 657 m² of land and is a house with three bedrooms and one bathroom.
How many parking spaces are provided at the residence?
The house includes one designated parking space for residents.
Which parks are located within a short walk from the property?
George Cross Park is about 0.1 km away, Legacy Park is roughly 0.3 km, and Victoria Cross Park is approximately 0.5 km from the home.
How close is the Australian War Memorial to 17 Jacka Crescent?
The Australian War Memorial is situated about 0.6 km from the property, a comfortable walking distance.
What war memorials can be found near the house?
Within 0.5–0.6 km you will find the Kemal Atatürk Memorial, Royal Australian Navy Memorial, Australian Army Memorial, Korean War Memorial, and Royal Australian Air Force Memorial.
Is the suburb of Campbell near any major roads or thoroughfares?
Yes, Anzac Parade runs close to the area, located about 0.6 km from the property.
What geological features characterize the Campbell area?
Campbell is mainly underlain by the lowest layer of the Ainslie Volcanics, consisting of grey dacite, agglomerate, and tuff, with higher layers of grey quartz andesite and cream rhyolite in the north and north‑east.