51 Katherine Avenue
51 Katherine Avenue, Amaroo ACT 2914, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Sep 2010 | $555,000 | $925 |
| Sold | Jun 2006 | $445,000 | $741 |
| Sold | Apr 2000 | $78,000 | $130 |
Price per m² based on land size of 600 m².
Key details
- Locality
- Amaroo
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714850436
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/AMAR/87/6
- Remoteness area
- Metro
- Property type
- House
- Land size
- 600 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
How many bedrooms and bathrooms does the house at 51 Katherine Avenue have?
The property features four bedrooms and two bathrooms. It is a standalone house offering ample space for a family.
What is the size of the land that the house sits on?
The home is set on a 600 m² block. The size provides room for a garden or outdoor entertaining area.
What parking facilities are available at this address?
The property includes two off‑street parking spaces. These are provided as part of the house’s amenities.
What does the name ‘Amaroo’ mean?
Amaroo is derived from the Nyoongar language and means “a beautiful place.” The suburb’s name reflects its pleasant surroundings.
How far is 51 Katherine Avenue from the Gungahlin Town Centre?
The residence is located approximately 1.4 km (about 1–2 km) from the Gungahlin Town Centre, offering easy access to shops and services.
What nearby parks, lakes or shopping centres can I reach on foot?
Yerrabi Pond is about 0.8 km away, Crinigan Park roughly 1.3 km distant, and the Gungahlin Marketplace shopping centre is around 1.7 km from the property. All are within a short walking distance.
What are the main geological features of the Amaroo area?
Amaroo sits on the Canberra Formation, predominantly composed of slaty shale and mudstone, with a central band of dacite and quartz‑andesite. The terrain shows north‑north‑east folding and a few short faults marked by quartz.