16 Paul Coe Crescent
16 Paul Coe Crescent, Ngunnawal ACT 2913, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Nov 2006 | $350,000 | $738 |
| Sold | Sep 1999 | $180,000 | $379 |
| Sold | Dec 1998 | $167,000 | $352 |
| Sold | Feb 1995 | $42,000 | $88 |
Price per m² based on land size of 474 m².
Key details
- Locality
- Ngunnawal
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714903746
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/NGUN/100/29
- Remoteness area
- Metro
- Property type
- House
- Land size
- 474 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 are the main internal features of the home at 16 Paul Coe Crescent?
The property is a house with four bedrooms and two bathrooms. It also includes two parking spaces for vehicles.
How large is the land on which the house is situated?
The house sits on a 474 m² block, offering ample outdoor space for gardening or recreation.
How far is the property from the nearest major town centres?
Ngunnawal is located about 4 km from the Gungahlin Town Centre and roughly 13 km from the centre of Canberra, providing convenient access to city amenities.
Which parks are within easy walking distance of the home?
Several parks are nearby: Crinigan Park (≈0.5 km), Ginninderra Park (≈0.7 km), Violets Park (≈0.8 km), and Girrawah Park (≈1.0 km) are all within a short walk.
What community facilities are close to the residence?
The Gold Creek Homestead is about 1.4 km away, and the Gungahlin Enclosed Oval, a local stadium, is roughly 1.3 km from the property, offering recreational options.
What geological features underpin the Ngunnawal area?
The suburb sits on the Canberra Formation, mainly composed of slaty shale and mudstone, with pockets of dacite, quartz andesite, and tuff outcrops. The rock structure includes north‑north‑east aligned folds and the Deakin Fault runs near Ginninderra Creek.