100 Hugh Mckay Crescent
100 Hugh Mckay Crescent, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jun 2022 | — | — |
Price per m² based on land size of 854 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714848374
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/21/55
- 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
- 854 m²
- Internal area
- 195 m²
- 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 are in the house at 100 Hugh Mckay Crescent?
The property offers five bedrooms and two bathrooms, providing ample space for families or guests.
What is the size of the land and the type of dwelling at this address?
It is a standalone house situated on an 854 m² block, giving a generous outdoor area surrounding the home.
How far is 100 Hugh Mckay Crescent from Canberra’s city centre?
The residence is located about 11.6 km (roughly 7 mi) north‑west of Canberra’s central business district.
What natural reserves or parks are close to this property?
Nearby natural attractions include the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all part of the Ginninderra Catchment.
Which nearby suburbs or estates are within walking distance of the home?
The house borders the suburbs of Fraser, Charnwood and Macgregor, and is part of the Dunlop Hills estate within the larger Dunlop suburb.
What geological features characterize the Dunlop area?
Dunlop sits on Silurian‑age rocks, primarily Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the southwest and the Deakin Fault running along its north‑east edge.