15 Conjola Close
15 Conjola Close, Amaroo ACT 2914, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2025 | $1,100,000 | — |
Key details
- Locality
- Amaroo
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714851537
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/AMAR/22/25
- Remoteness area
- Metro
- Property type
- House
- Internal area
- 265 m²
- 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 15 Conjola Close have?
The house offers four bedrooms and two bathrooms. It provides ample space for a medium‑sized family.
What is the price of the property?
The listed price for 15 Conjola Close is $1,100,000.
How many parking spaces are provided?
The property includes two parking spaces for residents.
How far is the home from the Gungahlin Town Centre?
Amaroo is situated about 1.4 km from the Gungahlin Town Centre, putting the home within a short walk or bike ride to shops and services.
Which parks are located nearby?
Crinigan Park is roughly 0.5 km away, while Ginninderra Park and Violets Park are each about 1.4 km from the house. Homestead Park is also close, at around 1.6 km.
What shopping options are available in the vicinity?
The Amaroo shopping precinct, featuring a Coles supermarket, Aldi, and other retailers, is nearby. Larger centres such as Gungahlin Marketplace and Gungahlin Village are also within easy reach.
Is there any historic site close to the property?
Yes, Crinigan's Hut Ruin, a remnant of the suburb’s colonial past, is located about 0.5 km away, offering a glimpse into the area’s history.
What geological features underlie the Amaroo area?
Amaroo sits on the Canberra Formation from the late middle Silurian age, primarily composed of slaty shale and mudstone with bands of dacite and quartz‑andesite. The local rock structure includes north‑north‑east folds and a few short faults marked by quartz.