61 Tarrant Crescent
61 Tarrant Crescent, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2005 | $352,000 | $782 |
| Sold | Jun 2000 | $40,500 | $90 |
| Sold | Jan 2000 | $179,500 | $398 |
Price per m² based on land size of 450 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847004
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/68/38
- Remoteness area
- Metro
- Property type
- House
- Land size
- 450 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 does the house have and what is the land size?
The property at 61 Tarrant Crescent offers four bedrooms and sits on a 450 m² block.
Where is 61 Tarrant Crescent located relative to Canberra city centre?
It is situated in the suburb of Dunlop, about 11.6 km north‑west of Canberra’s central business district.
What natural attractions are close to the property?
The home is adjacent to the Dunlop Grasslands Nature Reserve and near West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all part of the Ginninderra Catchment.
Which parks are near the residence?
The Boslem and Harte Park is roughly 1.2 km away and George Simpson Park is about 2 km distant, both providing playgrounds and walking/cycle paths.
What is the demographic profile of the Dunlop suburb?
According to the 2016 Census, Dunlop had around 7,200 residents, a median age of 33, and about 76 % of people were born in Australia.
Which local government electorate does the property fall under?
For ACT Legislative Assembly elections, Dunlop is in the Ginninderra electorate, and federally it is part of the Division of Fenner.
What geological features are characteristic of the area?
Dunlop sits on Silurian‑age volcanic rocks, primarily Deakin Volcanics purple rhyodacite, with grey tuff of the Laidlaw Volcanics in the south‑west and the Deakin Fault along its north‑east edge.