14 Connelly Place
14 Connelly Place, Belconnen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 1999 | $108,500 | $495 |
Price per m² based on land size of 219 m².
Key details
- Locality
- Belconnen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714865095
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/BELC/94/8
- Remoteness area
- Metro
- Property type
- House
- Land size
- 219 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 14 Connelly Place and how large is its land area?
14 Connelly Place is a house situated on a 219 m² parcel of land.
Which major commercial hub is nearest to the property?
The property is about 0.7 km from Belconnen Town Centre, the district’s primary shopping and services precinct.
What recreational facilities are within easy walking distance of the home?
Within 0.5–0.8 km you’ll find the Canberra International Sports & Aquatic Centre (0.3 km), a skateboard park (0.5 km), Margaret Timpson Park (0.8 km) and John Knight Memorial Park (0.9 km).
Which government offices are located close to 14 Connelly Place?
The Cameron Offices are about 0.4 km away and the Australian Bureau of Statistics is roughly 0.6 km from the property.
Are there public transport options nearby?
Belconnen Town Centre, about 0.7 km away, contains three bus stations providing regular services to the wider Canberra region.
What notable landmarks or public artworks can be found near the residence?
Nearby attractions include The Big Powerful Owl (0.6 km), the Tumbling Cubes sculpture in Margaret Timpson Park (0.8 km), and the Big Splash waterpark (0.8 km).
What geological features make the Belconnen area distinctive?
Belconnen sits at the intersection of the Deakin and Winslade faults, exhibiting a high density of volcanic rocks such as rhyodacite, dacite, and quartz‑andesite, along with various intrusions and shale formations.