36 William Webb Drive
36 William Webb Drive, Evatt ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2012 | $450,000 | $627 |
| Sold | Nov 2007 | $400,000 | $557 |
Price per m² based on land size of 717 m².
Key details
- Locality
- Evatt
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714850974
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/EVAT/23/6
- 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
Frequently asked questions
What are the main features of the home at 36 William Webb Drive?
The property is a house offering three bedrooms and two bathrooms, set on a 717 m² block of land.
In which suburb and district is 36 William Webb Drive located?
It is situated in the suburb of Evatt, which forms part of the Belconnen district of Canberra, Australian Capital Territory.
What are the main roads that define the boundaries of Evatt?
Evatt is bordered by Copland Drive, Owen Dixon Drive, William Webb Drive and Ginninderra Drive.
What nearby facilities are within a short distance of the property?
Within roughly 0.4 km is Belconnen United FC, a local football club; the National Health Co‑op in Evatt is about 0.8 km away, and the National Dinosaur Museum can be reached in about 2 km.
Which electoral divisions does Evatt belong to?
For federal elections Evatt falls in the Division of Fenner, while for ACT Legislative Assembly elections it is part of the Ginninderra electorate.
When was the suburb of Evatt officially gazetted?
Evatt was officially gazetted on 2 November 1972.
What geological features are found beneath Evatt?
The area is dominated by a green‑grey dacitic intrusive porphyry with large white feldspar crystals, along with a Glebe Farm adamellite intrusion, green‑grey dacitic tuff in the south‑west, a segment of the Deakin fault, and a small patch of calcareous shale in the far southwest corner.