5 Revell Close
5 Revell Close, Gordon ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | May 2025 | $655,000 | $1,574 |
| Sold | Mar 2013 | $353,000 | $848 |
| Sold | Apr 2002 | $159,000 | $382 |
| Sold | May 1995 | $111,000 | $266 |
| Sold | Jul 1994 | $11,500 | $27 |
Price per m² based on land size of 416 m².
Key details
- Locality
- Gordon
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714856068
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/GORD/543/8
- Remoteness area
- Metro
- Property type
- House
- Land size
- 416 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
How many bedrooms are in the house at 5 Revell Close?
The property offers three bedrooms, providing ample space for a small family or shared living arrangements. Each bedroom is part of the single‑storey house layout.
What is the land area of the lot?
The house sits on a 416 m² block, giving enough room for a garden or outdoor entertaining area. The land size is typical for homes within the Gordon suburb.
Is there any on‑site parking available?
Yes, the property includes one designated parking space. This space is provided as part of the standard amenities for the house.
How close is the property to the nearest park?
Gordonvale Park is about 0.6 km away, and Beau and Jessi Park is roughly 0.8 km from the house. Both parks are within easy walking distance for recreation.
What is the distance to the neighboring suburb of Banks?
The suburb of Banks is situated approximately 0.6 km to the east of 5 Revell Close. It can be reached quickly by car or even on foot.
What geological features are found in Gordon?
In the south and centre of Gordon, Quaternary alluvium deposits are present, while the northern part of the suburb sits on Deakin Volcanics rhyodacitic crystal tuff from the Silurian age. These formations contribute to the local soil characteristics.