52 Keverstone Circuit
52 Keverstone Circuit, Isabella Plains ACT 2905, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Oct 2021 | $835,000 | $1,192 |
| Sold | Oct 2005 | $318,000 | $454 |
| Sold | Nov 2000 | $131,000 | $187 |
| Sold | May 1992 | $139,000 | $198 |
Price per m² based on land size of 700 m².
Key details
- Locality
- Isabella Plains
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714913730
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/ISAB/846/40
- Remoteness area
- Metro
- Property type
- House
- Land size
- 700 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 type of dwelling is located at 52 Keverstone Circuit?
It is a standalone house offering three bedrooms and one bathroom. The property provides a comfortable family‑size layout.
How much land does the house sit on?
The home is sited on a 700 m² block, giving ample outdoor space for gardening, recreation or future extensions.
What parking facilities are available for residents?
The property includes four designated parking spaces, allowing convenient vehicle accommodation for the household.
What shopping and community amenities are close to the property?
A small shopping centre on Ellerston Avenue and Galloway Street provides a supermarket, hairdresser, chemist, pathology clinic and takeaway. Adjacent to the shops is a neighbourhood centre with a car park, doctors’ surgery and community‑hire rooms.
How far is the automatic weather station from the house?
The Tuggeranong automatic weather station is located roughly 2 km away, offering local climate data for residents.
What is the underlying geology of Isabella Plains?
The suburb sits on Deakin Volcanics – green‑grey and purple rhyodacite from the Silurian period – which is overlain by alluvial deposits in the lower‑lying areas.