43 Abercorn Crescent
Isabella Plains ACT 2905, Australia
Snapshot
Key points for 43 Abercorn Crescent.
- Three bedrooms with a single bathroom
- Four parking spaces provided
- Located on a 1,230 m² parcel
- Standalone house layout
Key details
- Locality
- Isabella Plains
- State
- ACT
- Coordinates
- 35.42528401 / 149.10215619
- GNAF PID
- GAACT714923080
- Legal parcel ID
- TUGG/ISAB/886/62
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1230 m²
- Internal area
- -
- Land Use Category
- Residential
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sale | 24 Jul 2010 | $438,500 | $356 |
| Sale | 29 Oct 1998 | $107,500 | $87 |
| Sale | 30 Dec 1991 | $115,000 | $93 |
Price per m² based on land size of 1230 m².
Real Estate Agencies
Nearby schools
Frequently asked questions
What type of dwelling is located at 43 Abercorn Crescent?
It is a standalone house offering three bedrooms and one bathroom
How much land does the property at 43 Abercorn Crescent occupy?
The house sits on a 1,230 m² block, providing ample outdoor space
Which community facilities are within walking distance of 43 Abercorn Crescent?
A small shopping centre on Ellerston Avenue and Galloway Street provides a supermarket, hairdresser, pathology clinic, chemist and takeaway, plus a neighbourhood house and doctors surgery nearby
How close is the property to natural water features?
Tuggeranong Creek is approximately 0.4 km away, and Isabella Pond lies about 2 km from the home
What major roads define the boundaries of Isabella Plains?
The suburb is bounded by Isabella Drive, Drakeford Drive, Johnson Drive, and Ashley Drive
When was the suburb of Isabella Plains officially gazetted?
Isabella Plains was gazetted on 5 August 1975
What is the origin of the name ‘Isabella Plains’?
The name derives from Isabella Maria Brisbane, daughter of Governor Sir Thomas Brisbane, after early explorers referred to the area as ‘Isabella’s Plain’
What geological formation underlies the Isabella Plains area?
The suburb sits on Deakin Volcanics green‑grey and purple rhyodacite from the Silurian period, overlaid by alluvial deposits in lower‑lying parts
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