100 William Webb Drive
100 William Webb Drive, Evatt ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Feb 2003 | $227,500 | $253 |
| Sold | Jan 2002 | $99,500 | $110 |
| Sold | May 1997 | $112,000 | $124 |
| Sold | Nov 1993 | $137,000 | $152 |
Price per m² based on land size of 898 m².
Key details
- Locality
- Evatt
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714860765
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/EVAT/73/11
- Remoteness area
- Metro
- Property type
- House
- Land size
- 898 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 100 William Webb Drive?
It is a detached house situated on a residential block measuring 898 m².
How large is the land parcel for this house?
The property sits on a lot of approximately 898 square metres, providing ample garden and outdoor space.
In which suburb is the property and what are its neighbouring suburbs?
The house is in Evatt, a suburb of Canberra’s Belconnen district. Evatt lies between the suburbs of McKellar, Belconnen, Florey, Melba and Spence.
What major roads define the borders of Evatt?
Evatt is bounded by Copland Drive, Owen Dixon Drive, William Webb Drive and Ginninderra Drive.
What community facilities are located close to 100 William Webb Drive?
Within about 1 km you’ll find Evatt Primary School, Belconnen United Football Club, Copland College and the National Health Co‑op Evatt.
Which electoral divisions cover the suburb of Evatt?
For federal elections Evatt is in the Division of Fenner, and for ACT Legislative Assembly elections it falls within the Ginninderra electorate.
What are some of the notable geological features of Evatt?
The area is underlain by a green‑grey dacitic intrusive porphyry with large white feldspar crystals, the Glebe Farm Adamellite intrusion, dacitic tuff from the Hawkins Volcanics, a section of the Deakin fault, and a small patch of calcareous shale in the south‑west corner.