8 Tryon Street
8 Tryon Street, Hackett ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Feb 1996 | $205,000 | $285 |
| Sold | Jul 1991 | $215,000 | $299 |
Price per m² based on land size of 717 m².
Key details
- Locality
- Hackett
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714892537
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/HACK/36/10
- Remoteness area
- Metro
- Property type
- House
- Land size
- 717 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 have and what is the size of the land?
The property offers 4 bedrooms and 2 bathrooms. It sits on a 717 m² block, providing ample space for a family.
How far is the house from Canberra's central business district?
Hackett is located about 4.5 km north‑east of the Canberra CBD, making the city centre easily reachable by car.
What parks or natural reserves are close to the property?
Nearby green spaces include Calvert Park (approximately 1 km away), Justice Robert Hope Park (about 1.5 km), and Bill Pye Park (around 1.8 km). The suburb also borders the Mount Majura Nature Reserve to the east.
Is there public transport nearby?
The Officer Crescent bus shelter is located roughly 1.7 km from the house, providing access to local bus routes.
What shopping facilities are available in Hackett?
Hackett features a neighbourhood shopping centre within the suburb, just a short walk of about 0.4 km from the property.
What recreational facilities can residents use nearby?
Residents can enjoy the Dickson District Playing Fields (about 1.6 km away) and the nearby Dickson Wetland (around 1.7 km), offering sports and nature experiences.
What is the geological makeup of the Hackett area?
The suburb sits on calcareous shales from the Canberra Formation, overlain by Quaternary alluvium. The higher eastern side rests on the lowest layer of the Ainslie Volcanics, comprising grey dacite, agglomerate and tuff.