55 Handcock Crescent
55 Handcock Crescent, Macgregor ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2018 | $574,000 | — |
Key details
- Locality
- Macgregor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714883439
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/MACG/22/12
- Remoteness area
- Metro
- Property type
- House
- 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 and bathrooms does the home at 55 Handcock Crescent have?
The property offers three bedrooms and a single bathroom. It is a standalone house suitable for small families or couples.
What type of dwelling is located at 55 Handcock Crescent?
55 Handcock Crescent is a detached house. It provides private living space typical of the Macgregor residential area.
How many parking spaces are provided with the house?
The property includes two parking spaces. These can accommodate two vehicles on the premises.
Where is 55 Handcock Crescent situated within the suburb of Macgregor?
The home is located on Handcock Crescent in the suburb of Macgregor, which lies in the Belconnen district of Canberra. It is near the western edge of the suburb, close to the main thoroughfares Ginninderra Drive to the north and Southern Cross Drive to the south.
What natural features are close to 55 Handcock Crescent?
Goodwin Hill, a small mountain, is only about 0.3 km away, offering scenic views. The suburb also has Ginninderra Creek running through it for roughly 1.4 km.
Which parks are within walking distance of the property?
The Boslem and Harte Park is approximately 1.2 km away, and George Simpson Park is about 2 km distant, both providing green space and recreation options.
What geological formation underlies the Macgregor area where the house is located?
The suburb sits on Silurian‑age Deakin Volcanics, specifically purple rhyodacite, which forms the underlying bedrock of the area.