3 Gye Place
3 Gye Place, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2006 | $390,000 | $442 |
| Sold | Jul 2002 | $245,000 | $277 |
| Sold | Dec 1994 | $57,000 | $64 |
Price per m² based on land size of 882 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847002
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/13/9
- Remoteness area
- Metro
- Property type
- House
- Land size
- 882 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 3 Gye Place have?
The property offers four bedrooms and one bathroom.
What is the size of the land and the type of dwelling?
It sits on an 882 m² block and is a detached house.
How far is the property from Canberra’s city centre?
Dunlop is located about 11.6 km (approximately 7 mi) north‑west of Canberra’s central business district.
What natural reserves or ponds are nearby?
The suburb borders the Dunlop Grasslands Nature Reserve and is close to West Belconnen Ponds, Jarramlee Pond and Fassifern Pond within the Ginninderra Catchment.
Which neighbouring suburbs are closest to 3 Gye Place?
It is adjacent to Fraser, Charnwood (about 1.7 km away) and Macgregor (approximately 1.4 km away).
What parks or recreational areas are within a short distance?
The Boslem and Harte Park is around 1.5 km away, and George Simpson Park lies about 2.5 km from the property, both offering open space for walking and leisure.
Is there a notable geographic feature close to the house?
Goodwin Hill, a local mountain, is situated roughly 1.1 km from the property.
What is the geological composition of the Dunlop area?
The land is primarily made up of Silurian‑age Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west and Hawkins Volcanics uplifted along the Deakin Fault.