2 Akubra Place
2 Akubra Place, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Built | — | — |
Price per m² based on land size of 500 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847698
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/102/1
- Commonwealth electorate
The federal electorate this address is in (for Australia's Parliament).
- Fenner
- State lower house
The state electorate this address is in (lower house).
- Ginninderra
- Remoteness area
- Metro
- Property type
- House
- Land size
- 500 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 type of property is located at 2 Akubra Place and what are its main specifications?
It is a standalone house set on a 500 m² block, offering four bedrooms and two bathrooms.
How far is 2 Akubra Place from Canberra’s city centre?
The property is situated about 11.6 km north‑west of the Canberra central business district.
What natural reserves or water features are nearby the property?
Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond are located within or adjacent to the suburb.
Which park is located close to 2 Akubra Place?
The Boslem And Harte Park lies approximately 1.7 km from the home.
What is the origin of the street name Akubra Place?
Akubra refers to an iconic Australian hat brand, with the name believed to derive from an Aboriginal word for head covering.
In which political divisions does the property belong?
Federally the property is in the Division of Fenner, and for ACT Legislative Assembly elections it is part of the Ginninderra electorate.
What are the key geological characteristics of the Dunlop area?
The suburb sits on Silurian‑age rocks, predominantly Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west and the Deakin Fault running along its north‑east edge.