78 Keverstone Circuit
78 Keverstone Circuit, Isabella Plains ACT 2905, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Built | Unknown | — |
Price per m² based on land size of 788 m².
Key details
- Locality
- Isabella Plains
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714911242
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/ISAB/846/16
- Remoteness area
- Metro
- Property type
- House
- Land size
- 788 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 land size of the property at 78 Keverstone Circuit?
The house sits on a 788 m² block, providing ample garden and outdoor space.
How many bedrooms and bathrooms does this home have?
The residence offers four bedrooms and two bathrooms, suitable for a medium‑size family.
Where is 78 Keverstone Circuit located within Canberra?
It is situated in the suburb of Isabella Plains in the Tuggeranong district, bounded by Isabella Drive, Drakeford Drive, Johnson Drive and Ashley Drive.
What community facilities are nearby the property?
A small shopping centre with a supermarket, hairdresser, pharmacy and takeaway is on the corner of Ellerston Avenue and Galloway Street, and a neighbourhood house and doctors’ surgery are located opposite the shops.
What natural attractions are close to the home?
Within roughly 2 km you can reach Barneys Hill, Isabella Pond, Stranger Pond, Pine Island Reserve and Lake Tuggeranong, offering opportunities for walking, fishing and picnics.
Is there a weather monitoring station nearby?
Yes, the Tuggeranong automatic weather station (TUGGERANONG ISABELLA PLAINS AWS) is about 1.8 km away.
What is the geological makeup of the Isabella Plains area?
The suburb sits on Deakin Volcanics green‑grey and purple rhyodacite from the Silurian period, overlaid in the lower‑lying parts by alluvial deposits.