32 Burdekin Avenue
32 Burdekin Avenue, Amaroo ACT 2914, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jan 1998 | $180,000 | $245 |
| Sold | May 1997 | $58,000 | $79 |
Price per m² based on land size of 733 m².
Key details
- Locality
- Amaroo
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714848911
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/AMAR/6/2
- Remoteness area
- Metro
- Property type
- House
- Land size
- 733 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 is the land size of the property at 32 Burdekin Avenue?
The property sits on a 733 m² block. It is a detached house occupying this land area.
How close is 32 Burdekin Avenue to the Gungahlin Town Centre?
The suburb of Amaroo is approximately 1.4 km from the Gungahlin Town Centre, placing the house just a short drive or walk away.
Which parks are within walking distance of the house?
Nearby green spaces include Crinigan Park (about 0.3 km away), Violets Park and Girrawah Park (around 1.2‑1.6 km), and Ginninderra Park roughly 1.4 km from the property.
What historic sites are close to 32 Burdekin Avenue?
The historic Crinigan's Hut Ruin lies only 0.2 km away, and the remains of Crinigan’s stone cottage from the 1840s are a short distance further, highlighting the area’s colonial past.
Is high‑speed NBN internet available in Amaroo?
Yes. Amaroo was the first suburb in the ACT to receive 100 Mbps NBN service, with the rollout completed in 2013.
What shopping facilities are nearby?
An Amaroo shopping precinct on Horsepark Drive offers a Coles supermarket, Aldi, Wok it Up and other retailers, and larger centres such as Gungahlin Marketplace and Gungahlin Village are also close by.
What geological features underlie the Amaroo area?
Amaroo sits on the Canberra Formation from the late middle Silurian age, mainly composed of slaty shale and mudstone, with a central band of dacite and quartz‑andesite, a small tuff patch, and folded structures marked by short faults.