4 Bartels Place
4 Bartels Place, Banks ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Dec 2016 | $496,000 | $672 |
| Sold | Feb 2002 | $165,000 | $223 |
| Sold | Aug 2000 | $128,000 | $173 |
| Sold | Jun 1998 | $105,000 | $142 |
| Sold | Apr 1993 | $129,950 | $176 |
Price per m² based on land size of 737 m².
Key details
- Locality
- Banks
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714850983
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/BANK/46/31
- Remoteness area
- Metro
- Property type
- House
- Land size
- 737 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 type of property is located at 4 Bartels Place and how many bedrooms does it have?
4 Bartels Place is a house that features three bedrooms. It also includes a single bathroom and sits on a spacious block.
How large is the land area for the house at 4 Bartels Place?
The property sits on a 737 m² land parcel, providing ample outdoor space within the suburb of Banks.
What parking options are available at 4 Bartels Place?
The dwelling offers two parking spaces for residents, allowing convenient vehicle accommodation.
What local amenities are near 4 Bartels Place?
A small shopping centre on Pockett Avenue is close by, featuring a SUPAEXPRESS supermarket, two take‑away food shops, and a pet grooming shop. Beau and Jessi Park and Gordonvale Park are also within a short walk.
What natural attractions can be found near the property?
The Rob Roy Nature Reserve lies to the east of Banks, offering hilly terrain and views of Mt Rob Roy. Nearby, the smaller mountain Big Monks provides a gliding stage for paragliders and hang‑gliders.
What is the underlying geology of the Banks suburb where the house is located?
The surface geology of Banks is alluvium, while the surrounding hills are composed of Deakin Volcanics that erupted during the Silurian age, about 414 million years ago.