8 Grove Place
8 Grove Place, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2008 | $435,000 | $902 |
| Sold | May 2001 | $204,000 | $423 |
| Sold | Mar 2000 | $46,000 | $95 |
Price per m² based on land size of 482 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847990
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/20/28
- Remoteness area
- Metro
- Property type
- House
- Land size
- 482 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 8 Grove Place and how large is the land?
8 Grove Place is a house situated on a 482 m² parcel of land.
Where is 8 Grove Place positioned within Canberra?
The property is in the suburb of Dunlop, part of the Belconnen district, about 11.6 km north‑west of Canberra’s city centre.
What natural reserves or parks are close to the property?
Nearby are the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, with The Boslem and Harte Park roughly 2 km away.
How far is the nearest weather station from 8 Grove Place?
The Ginnindera weather station in Charnwood is approximately 0.8 km from the property.
What is the origin of the suburb name ‘Dunlop’?
Dunlop is named after Lieutenant Colonel Sir Ernest Edward “Weary” Dunlop, an Australian surgeon renowned for his leadership while a prisoner of war during the Second World War.
Which electoral divisions does Dunlop belong to?
For ACT Legislative Assembly elections Dunlop is in the Ginninderra electorate, and for federal elections it falls within the Division of Fenner.
What geological features characterize the Dunlop area?
Dunlop sits on Silurian‑age rocks, mainly 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.