110 Hugh Mckay Crescent
110 Hugh Mckay Crescent, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Apr 2001 | $145,950 | $461 |
| Sold | Nov 2000 | $41,000 | $129 |
Price per m² based on land size of 316 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714848402
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/23/21
- Remoteness area
- Metro
- Property type
- House
- Land size
- 316 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 home is located at 110 Hugh Mckay Crescent?
It is a detached house featuring three bedrooms and one bathroom. The property sits on a 316 m² block and includes one parking space.
How far is Dunlop from Canberra's city centre?
Dunlop lies about 11.6 kilometres (approximately 7 miles) north‑west of Canberra’s central business district, offering a short drive to the city.
What natural reserves or water features are close to the property?
The suburb borders the Dunlop Grasslands Nature Reserve and is near West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all part of the Ginninderra Catchment.
Which parks are within walking distance of 110 Hugh Mckay Crescent?
The Boslem and Harte Park is roughly 1.8 km away, providing open green space and walking tracks for residents.
Where can I find shopping and community facilities nearby?
Kippax Fair Shopping Centre and the Kippax Centre are each about 2.5 km from the home, offering retail, services and dining options.
What electoral divisions does Dunlop belong to?
For federal elections, Dunlop is part of the Division of Fenner. In the ACT Legislative Assembly, it falls within the Ginninderra electorate.
What is the geological composition of the Dunlop area?
The suburb sits on Silurian‑age rocks, primarily Deakin Volcanics purple rhyodacite, with pockets of grey tuff from the Laidlaw Volcanics in the south‑west and the Deakin Fault along the north‑east edge.