16 Kirkwood Crescent
16 Kirkwood Crescent, Gordon ACT 2906, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2017 | $900,000 | $965 |
| Sold | Sep 2004 | $590,000 | $633 |
| Sold | May 2002 | $472,500 | $506 |
| Sold | Apr 1997 | $65,000 | $69 |
| Sold | Jan 1993 | $66,000 | $70 |
Price per m² based on land size of 932 m².
Key details
- Locality
- Gordon
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714852288
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/GORD/505/28
- Remoteness area
- Metro
- Property type
- House
- Land size
- 932 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 residence is located at 16 Kirkwood Crescent?
It is a detached house offering family living space. The property is situated on a 932 m² block.
How many bedrooms and bathrooms does the home have?
The house features five bedrooms and three bathrooms, providing ample accommodation for a larger household.
What is the size of the land parcel for this property?
The residence sits on a land area of 932 m², allowing for a sizable garden or outdoor area.
Where is Gordon suburb located within the Canberra region?
Gordon is a suburb in the Tuggeranong district of Canberra, positioned on the west side of Tharwa Drive with postcode 2906.
What parks or recreational areas are close to 16 Kirkwood Crescent?
Gordonvale Park is about 0.8 km away, Beau and Jessi Park is roughly 1.7 km distant, and the Point Hut Pond and its district park lie within the suburb.
How far is the property from neighboring suburbs such as Conder and Banks?
Conder is approximately 1.4 km away, while Banks is about 1.7 km distant, making nearby amenities easily reachable.
What geological features are present in the Gordon area?
The southern and central parts of Gordon contain Quaternary alluvium, whereas the northern section is covered by Silurian‑age Deakin Volcanics rhyodacitic crystal tuff.