39 Hugh Mckay Crescent
39 Hugh Mckay Crescent, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2000 | $136,500 | $299 |
| Sold | Apr 1996 | $124,000 | $271 |
| Sold | Nov 1995 | $39,000 | $85 |
Price per m² based on land size of 456 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714848435
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/30/2
- Remoteness area
- Metro
- Property type
- House
- Land size
- 456 m²
- Internal area
- -
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Real Estate Agencies
Frequently asked questions
What type of residence is located at 39 Hugh Mckay Crescent?
It is a detached house featuring three bedrooms. The property sits on a 456 m² land parcel.
How far is the suburb of Dunlop from Canberra’s city centre?
Dunlop lies about 11.6 km north‑west of Canberra’s central business district, roughly a 15‑minute drive.
Which nature reserves or ponds are close to this address?
Nearby natural areas include the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all within the Ginninderra Catchment.
What estates are found within the Dunlop suburb?
Dunlop comprises several distinct estates: The Meadows, Ginninderra Ridge, Ginninderra Ponds, Dunlop Hills and Jarramlee Park.
What is the theme behind many of Dunlop’s street names?
Streets are named after Australian inventors, inventions and artists, such as Buckmaster Crescent (artist), Evelyn Owen Crescent (submachine‑gun designer) and Lance Hill Avenue (creator of the Hills hoist).
Which electoral divisions cover Dunlop?
Federally, Dunlop is part of the Division of Fenner. For ACT Legislative Assembly elections, it falls in the Ginninderra electorate.
What geological features are characteristic of Dunlop?
The area sits on Silurian‑age rocks, primarily Deakin Volcanics’ purple rhyodacite, with grey tuff in the south‑west and the Deakin Fault along the north‑east edge. Nearby uplifted Hawkins Volcanics include green‑grey dacite and quartz‑andesite.