31 Clifford Crescent
31 Clifford Crescent, Melba ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Nov 2024 | $675,000 | $642 |
| Sold | Aug 2020 | $610,000 | $580 |
| Sold | Feb 1992 | $108,000 | $102 |
Price per m² based on land size of 1050 m².
Key details
- Locality
- Melba
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714874245
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/MELB/20/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1050 m²
- Internal area
- 120 m²
- 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 dwelling is located at 31 Clifford Crescent?
It is a standalone house featuring four bedrooms and one bathroom.
How much land does the property occupy?
The house sits on a 1,050 m² block, providing ample outdoor space.
What parking provisions are included with the home?
The property offers two parking spaces for residents and guests.
What recreational facilities are close to 31 Clifford Crescent?
The Melba Tennis Club with eight courts is adjacent to the playing fields, George Simpson Park is about 1‑2 km away, and Belconnen United FC is roughly 2 km from the house.
Where is the nearest health service to this address?
The National Health Co‑op in Evatt is situated approximately 1 km from the property.
Why is the suburb of Melba named as such?
Melba is named after Dame Nellie Melba, Australia’s first internationally recognised opera soprano, and its streets honor composers, singers and other notable musical figures.
Which electoral divisions cover the Melba area?
For federal elections Melba falls within the Division of Fenner, and for ACT Legislative Assembly elections it is part of the Ginninderra electorate.
What notable geological features are found in Melba?
The suburb contains a porphyry of green‑grey dacitic intrusive with large white feldspar crystals, green‑grey dacitic tuff from the Hawkins Volcanics, and an intrusion of the Deakin Fault marked by quartz.