14 Alarmon Crescent
14 Alarmon Crescent, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Apr 2000 | $32,500 | $92 |
Price per m² based on land size of 352 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714847008
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/14/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 352 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
How many bedrooms and bathrooms does the house at 14 Alarmon Crescent have?
The home features four bedrooms and two bathrooms. This layout provides ample space for families or guests.
What is the size of the land the property sits on?
The house sits on a 352 m² block. The size offers room for a garden or outdoor entertaining area.
How many parking spaces are available at the property?
The property includes two parking spaces. These are provided on the site for convenient vehicle storage.
What nature reserves or parks are located near 14 Alarmon Crescent?
Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond are all within the suburb. The Boslem And Harte Park is also nearby, roughly 1.5 km away.
How far is the house from Canberra's city centre?
The property is situated about 11.6 km north‑west of Canberra's central business district. This places it within a short drive of the city’s main amenities.
Who was the suburb of Dunlop named after?
Dunlop is named after Lieutenant Colonel Sir Ernest Edward “Weary” Dunlop, an Australian surgeon renowned for his leadership as a prisoner of war during World War II.
What geological features are characteristic of the Dunlop area?
The suburb sits on Silurian‑age rocks, primarily Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west. The Deakin Fault runs along the north‑east edge of Dunlop, where green‑grey dacite and quartz‑andesite of the Hawkins Volcanics are uplifted.