15 Macintyre Place
15 Macintyre Place, Charnwood ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2025 | $758,000 | $847 |
| Sold | Apr 1994 | $127,500 | $142 |
| Sold | Sep 1991 | $115,000 | $128 |
Price per m² based on land size of 894 m².
Key details
- Locality
- Charnwood
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714846808
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/CHAR/111/9
- Remoteness area
- Metro
- Property type
- House
- Land size
- 894 m²
- Internal area
- 123 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 the house have?
The property features three bedrooms and two bathrooms.
What is the size of the land the house sits on?
The residence sits on a block of approximately 894 m².
What park is closest to the property?
The Boslem And Harte Park is right on the doorstep, essentially adjacent to the home.
What shopping options are nearby?
The Charnwood centre shopping area is about half a kilometre away and includes fast‑food outlets, a Woolworths supermarket, a Shell service station and the local Labor Club.
Is there an emergency services facility close to the home?
Yes, an emergency services station offering ambulance, fire and rescue services is located near the Charnwood shops at the south‑west corner of Lhotsky Street and Tillyard Drive.
How was the suburb of Charnwood originally designed?
Charnwood was planned using the Radburn principle, with houses originally intended to face shared parkland and garages positioned at the rear, though later fence building has altered that layout.
What geological features are found in the Charnwood area?
The suburb sits on Silurian‑age rocks, mainly Deakin Volcanics purple rhyodacite, with Hawkins Volcanics green‑grey dacite and quartz‑andesite nearby, and the Deakin Fault runs along the north‑east edge of these formations.