23 Alarmon Crescent
23 Alarmon Crescent, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jun 1994 | $121,000 | $252 |
| Sold | Jun 1990 | $41,000 | $85 |
Price per m² based on land size of 480 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847183
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/15/11
- Remoteness area
- Metro
- Property type
- House
- Land size
- 480 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 type of dwelling is located at 23 Alarmon Crescent?
It is a house situated on a 480 m² residential block.
Where is 23 Alarmon Crescent positioned within Canberra?
The address is in Dunlop, a suburb of the Belconnen district, about 11.6 km north‑west of Canberra’s city centre and near the ACT/NSW border.
What natural reserves are close to the property?
Dunlop contains the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all offering walking tracks and wildlife habitats within easy reach.
How far are the nearest parks from 23 Alarmon Crescent?
The Boslem And Harte Park is roughly 1.4 km away, while George Simpson Park lies about 2‑3 km from the property.
Which neighbouring suburbs are nearby and how far are they?
Fraser, Charnwood and Macgregor border Dunlop; Macgregor is about 1.4 km away and Charnwood around 1.6 km from the address.
What does the demographic profile of Dunlop look like?
According to the 2016 census, Dunlop had around 7,200 residents, a median age of 33 years, and about 76 % of people were born in Australia.
What geological features are characteristic of the Dunlop area?
The suburb sits on Silurian‑age Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west and the Deakin Fault running along its north‑east edge.