64 Barada Crescent
64 Barada Crescent, Aranda ACT 2614, Australia
Key details
- Locality
- Aranda
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714859134
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/ARAN/28/17
- Remoteness area
- Metro
- Property type
- House
- Land size
- 905 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 property is located at 64 Barada Crescent?
It is a house situated on a 905 m² parcel of land. The property offers a spacious footprint within the Aranda suburb.
How close is the property to the nearest park or natural reserve?
Aranda Bushland is the closest park, located about 0.3 km away. This provides easy access to walking tracks and native bushland scenery.
What public transport options are available near the property?
ACTION bus route 32 serves the area, linking residents to Civic and Belconnen Town Centre. A bicycle path along Bindubi Street also connects to the wider Canberra bike network.
Which community amenities are within walking distance of the house?
The Jamison Centre shopping mall, the National Health Co‑op, and Calvary Public Hospital in Bruce are all roughly 1.3–1.4 km away. Local Aranda shops, a newly opened café and bar also serve the neighbourhood.
What is the natural environment like in Aranda?
Aranda is characterised by a bush setting with large native eucalypt trees retained from its original landscape. The suburb is bounded on two sides by nature park and sits at the western foot of Black Mountain.
How did the suburb of Aranda get its name?
The name comes from the Arrernte (formerly Arunta) tribe of Central Australia, meaning “White Cockatoo”. Street names in the area honour Aboriginal tribal groups from across Australia.
What geological features underlie the land at 64 Barada Crescent?
The site sits on the Pittman Formation, an upper Ordovician greywacke rock, with bands of Acton Shale that contain graptolites. The Deakin Fault runs nearby, separating these rocks from Silurian‑age Mount Painter Volcanics to the southwest.