19 Moonbi Crescent
19 Moonbi Crescent, Isabella Plains ACT 2905, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Oct 1995 | $129,500 | $173 |
| Sold | Mar 1991 | $104,000 | $139 |
Price per m² based on land size of 745 m².
Key details
- Locality
- Isabella Plains
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714916222
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/ISAB/816/5
- Remoteness area
- Metro
- Property type
- House
- Land size
- 745 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 kind of dwelling is located at 19 Moonbi Crescent?
It is a standalone house situated on a 745 m² block.
How large is the land parcel for this property?
The house sits on approximately 745 square metres of land.
What shopping options are available nearby?
A small shopping centre on the corner of Ellerston Avenue and Galloway Street provides a supermarket, hairdresser, pathology clinic, chemist and a takeaway shop, all within a short walk.
Which community facilities can residents access close to the property?
Residents can use the neighbourhood house, a doctors surgery opposite the shops, a neighbourhood centre with a car park that hosts playgroups, and an early childhood centre offering day‑care and health services.
What churches are located within a few kilometres of the address?
Alliance Church Calwell is about 1.4 km away and Sacred Heart Church in Calwell is roughly 1.9 km distant.
What natural features are near 19 Moonbi Crescent?
Tuggeranong Creek runs about 0.7 km from the property, Isabella Pond lies roughly 2 km away, and Barneys Hill is situated approximately 1.9 km to the southeast.
What is the underlying geology of the Isabella Plains area?
The suburb rests on Deakin Volcanics green‑grey and purple rhyodacite from the Silurian period, which is overlain by alluvial deposits in the lower‑lying sections.