35 Evelyn Owen Crescent
35 Evelyn Owen Crescent, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jan 1995 | $104,850 | $211 |
Price per m² based on land size of 496 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847227
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/8/11
- Remoteness area
- Metro
- Property type
- House
- Land size
- 496 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 are the main features of the house at 35 Evelyn Owen Crescent?
It is a house offering 3 bedrooms, 2 bathrooms, a single parking space and sits on a 496 m² block of land.
How far is the property from Canberra’s city centre?
The home is located about 11.6 km north‑west of Canberra’s central business district.
Which nature reserves or ponds are close to the property?
Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond lie at the edge and within the suburb, making them very nearby.
What parks are within a short walk of 35 Evelyn Owen Crescent?
The Boslem And Harte Park is roughly 1.2 km away, while George Simpson Park is about 2.2 km distant, and the suburb also has several local playgrounds.
Which suburbs border Dunlop?
Dunlop is adjacent to Fraser, Charnwood and Macgregor, with Latham located a short distance away as well.
What is the origin of the street name Evelyn Owen Crescent?
Evelyn Owen Crescent is named after Evelyn Ernest Owen, the Australian inventor of the Owen Submachine Gun used in the Second World War, Korean War and Vietnam War.
What geological characteristics does the Dunlop area have?
The suburb sits on Silurian‑age rocks, dominated by Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the southwest and the Deakin Fault running along its north‑east edge.