59 Sullivan Crescent
Wanniassa ACT 2903, Australia
Key details
- Locality
- Wanniassa
- State
- ACT
- Coordinates
Latitude and longitude for the mapped property location.
- 35.39708563 / 149.10060896
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714941605
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/WANN/227/11
- Remoteness area
- Metro
- Property type
- House
- Land size
- 979 m²
- Internal area
- 170 m²
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sale | 29 Mar 1993 | $240,000 | $245 |
Price per m² based on land size of 979 m².
Real Estate Agencies
Nearby schools
Frequently asked questions
How many bedrooms and bathrooms are there at 59 Sullivan Crescent?
The house offers four bedrooms and two bathrooms, providing ample space for a family
What is the size of the land on which the property sits?
The residence is set on a 979 m² block, giving plenty of room for outdoor activities and potential landscaping
Which shopping centres are closest to the home?
Erindale Centre is about 0.7 km away and provides a range of retail and service outlets, while the smaller Wanniassa Shops are also within the suburb, offering a Coles supermarket and local businesses
What public transport options are available in Wanniassa?
Wanniassa is served by ACTION bus routes, including the R5 route to Civic via Woden Town Centre, and routes 72‑77 that connect the suburb to Tuggeranong Town Centre
What recreational facilities are located near the property?
Nearby amenities include the Erindale Vikings Club, Active Leisure Centre, Erindale Theatre, Erindale Library, and sporting venues such as the Wanniassa Enclosed Oval and Erindale tennis courts, all within roughly 1 km
What is the geological makeup of the Wanniassa area?
The suburb sits on Deakin Volcanics from the Silurian period, about 414 million years old, featuring cream‑green and purple rhyodacite in the eastern half and tuff, agglomerate, and rhyolite in the western part
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