53 Bennelong Crescent
53 Bennelong Crescent, Macquarie ACT 2614, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2019 | $572,500 | $792 |
| Sold | Apr 1998 | $105,500 | $146 |
Price per m² based on land size of 722 m².
Key details
- Locality
- Macquarie
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714875135
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/MACQ/22/15
- Remoteness area
- Metro
- Property type
- House
- Land size
- 722 m²
- Internal area
- 127 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
How many bedrooms and bathrooms does 53 Bennelong Crescent have?
The property features three bedrooms and two bathrooms, providing ample space for a family.
What is the size of the land the house sits on?
The house is situated on a 722 m² block, offering a generous outdoor area.
How close is the property to Macquarie Primary School?
Macquarie Primary School is located on the same street, essentially 0 km away, giving immediate access for residents.
What shopping options are available nearby?
The major Jamison Centre shopping mall is about 1.2 km away, and a smaller local centre on Lachlan Street with a medical centre, chemist, coffee shop and Vietnamese restaurant is within the suburb.
Which public transport serves the Macquarie area?
ACTION bus route 32 connects Macquarie with Belconnen Town Centre and Civic, providing convenient public‑transport links.
What recreational facilities are close to the house?
Big Splash, a public swimming pool with an outdoor water slide, is roughly 1 km away, and the playing fields adjacent to Canberra High School are about 1.4 km from the property.
Are there any notable geological features in the suburb?
The eastern side of Macquarie contains greywacke from the Ordovician Pittman Formation uplifted along the Deakin Fault, while green‑grey rhyodacite of the Walker Volcanics underlies the centre and western areas.