62 Forsythe Street
62 Forsythe Street, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2004 | $190,000 | $261 |
| Sold | Sep 2002 | $125,000 | $172 |
Price per m² based on land size of 726 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714854393
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/115/31
- Remoteness area
- Metro
- Property type
- House
- Land size
- 726 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 62 Forsythe Street?
It is a house situated on a 726 m² residential lot. The property is in the suburb of Banks, ACT.
How large is the land parcel for this house?
The land size is 726 m², providing a moderate block for a single‑family home. It sits within the gently sloping terrain of Banks.
What parks and recreational areas are close to 62 Forsythe Street?
Beau and Jessi Park and Gordonvale Park are both about 0.7 km away, offering green space and walking trails. The suburb’s own Banks Oval, used for community sports, is also nearby.
Is there a shopping centre in the vicinity of the property?
Yes, a small shopping centre on Pockett Avenue is within walking distance. It includes a SUPAEXPRESS supermarket, two take‑away food shops and a pet grooming salon.
What natural features or reserves are located near the house?
To the east of Banks lies the Rob Roy Nature Reserve, part of Canberra Nature Park, and the smaller Big Monks mountain with a gliding stage for paragliders. Both areas are accessible within a few kilometres of the property.
What is the underlying geology of the Banks suburb where the house is located?
The surface geology consists of alluvium across the whole suburb. Beneath the alluvium, the surrounding hills are formed of Deakin Volcanics, volcanic rocks that erupted during the Silurian period about 414 million years ago.