5 Mcaulay Place
5 Mcaulay Place, Florey ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2001 | $183,000 | $299 |
| Sold | Feb 1999 | $162,500 | $265 |
| Sold | Oct 1993 | $160,000 | $261 |
Price per m² based on land size of 612 m².
Key details
- Locality
- Florey
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714862327
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/FLOR/74/9
- Remoteness area
- Metro
- Property type
- House
- Land size
- 612 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 size of the land parcel at 5 Mcaulay Place?
The property sits on a 612 m² block. It is a detached house occupying that land area.
How close is the property to Belconnen Town Centre?
5 Mcaulay Place is about 0.7 km from Belconnen Town Centre, making it a short walk or quick drive to the district’s main commercial hub.
Which public transport options serve the area around the property?
Florey is serviced by three ACTION bus routes – Route 2, Route 3 and Route 40 – providing regular connections to nearby suburbs and the town centre.
Are there any notable community or cultural facilities nearby?
The Hindu Temple and Cultural Centre on Ratcliffe Crescent is just a short distance away, and the Florey shopping centre on Kesteven Street offers local shops and a commemorative bronze plaque about Lord Florey.
What recent environmental improvements have been made in the locality?
In 2018, the ACT Healthy Waterways Project restored sections of the drainage channel along Tattersall Crescent, returning it to a more natural creek‑like state to help slow and clean stormwater flowing into Ginninderra Creek.
What is the geological composition of the area surrounding the property?
The suburb sits on Silurian‑age rocks, including green‑grey dacite and quartz‑andesite of the Hawkins Volcanics, calcareous shale from the Yass Subgroup, and various rhyodacite and rhyolite formations.