62 Longstaff Street
62 Longstaff Street, Lyneham ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 1997 | $184,000 | $316 |
Price per m² based on land size of 581 m².
Key details
- Locality
- Lyneham
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714893733
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/LYNE/27/2
- Remoteness area
- Metro
- Property type
- House
- Land size
- 581 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 62 Longstaff Street?
It is a standalone house with four bedrooms set on a 581 m² block.
How large is the land parcel for this property?
The property sits on 581 square metres of land, providing ample garden or development space.
Which local attractions are within walking distance of the house?
The historic Old Canberra Inn is about 0.2 km away, the National Hockey Centre 0.3 km, St Ninian's Church 0.4 km, and Tilley's Café roughly 0.7 km from the house.
What public transport options are close to 62 Longstaff Street?
Light rail stations such as Dickson Interchange and Swinden Street are about 0.9 km away, and several bus routes (R9, 30, 31, 50, 51) serve the area.
What recreational facilities are nearby?
Exhibition Park in Canberra (EPIC) hosts events like Summernats, and sports venues including the National Hockey Centre and the ACT Netball Centre are within 0.3–0.5 km.
How would you describe the character and history of Lyneham?
Lyneham was gazetted in 1928 with development starting in 1958; it features leafy streets, a mix of 1960s homes and newer townhouses, and a strong community vibe centered around parks and cultural sites.
What is the underlying geology of the Lyneham area?
The suburb sits on Silurian calcareous shales from the Canberra Formation overlain by Quaternary alluvium, with Ordovician greywacke present in the north‑west.