26 Paul Coe Crescent
26 Paul Coe Crescent, Ngunnawal ACT 2913, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Feb 2019 | $460,000 | $1,064 |
| Sold | Jan 2009 | $365,000 | $844 |
| Sold | Jul 2006 | $325,000 | $752 |
| Sold | Dec 1998 | $127,500 | $295 |
| Sold | May 1995 | $35,000 | $81 |
Price per m² based on land size of 432 m².
Key details
- Locality
- Ngunnawal
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714907983
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/NGUN/100/14
- Remoteness area
- Metro
- Property type
- House
- Land size
- 432 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
How many bedrooms and bathrooms does the house at 26 Paul Coe Crescent have?
The property includes three bedrooms and two bathrooms, providing space for a small family or shared living arrangements.
What is the size of the land parcel for this house?
The house sits on a 432 m² block, offering a modest yard that can accommodate gardening or outdoor activities.
What parks are located within walking distance of the property?
Ginninderra Park and Crinigan Park are each about 0.6 km away, while Violets Park is roughly 0.8 km from the home, all easily reachable on foot.
How far is the property from the Gungahlin Town Centre and Canberra's city centre?
Ngunnawal is situated approximately 4 km from the Gungahlin Town Centre and about 13 km from the central business district of Canberra.
Are there any community facilities nearby, such as libraries or churches?
The Arabanoo Street Library is located within the suburb, and New Life Presbyterian Church can be found on Wanganeen Avenue, both a short drive from the property.
What notable geological features are present in the Ngunnawal area?
The suburb sits on the Canberra Formation, primarily composed of slaty shale and mudstone, with outcrops of dacite, quartz‑andesite, and tuff visible in various parts of the area.