13 Maranoa Street
13 Maranoa Street, Kaleen ACT 2617, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Nov 2025 | Unknown | — |
| Sold | Nov 2025 | Unknown | — |
Price per m² based on land size of 709 m².
Key details
- Locality
- Kaleen
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714874038
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/KALE/108/18
- Remoteness area
- Metro
- Property type
- House
- Land size
- 709 m²
- Internal area
- 176 m²
- 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 and bathrooms does the house at 13 Maranoa Street have?
The property offers four bedrooms and two bathrooms, providing ample space for a family or guests.
What is the size of the land on which the house sits?
The home occupies a 709 m² block, giving room for gardens, outdoor activities, or future extensions.
What parking facilities are available at this property?
The residence includes three parking spaces, offering convenient vehicle accommodation for residents.
What shopping options are located nearby?
Kaleen Plaza, a local shopping centre, is roughly 1 km away, and the suburb also has two smaller shopping strips along Maribyrnong Avenue.
Are there recreational or sports facilities close to 13 Maranoa Street?
Kaleen features several ovals, such as Kaleen North, Enclosed, District Playing Fields, and South ovals, supporting soccer, cricket, and rugby within a short distance of the property.
What cycling infrastructure exists in Kaleen?
The suburb is served by a well‑maintained network of bicycle paths, including a main north‑south track that passes under Ginninderra Drive and runs through the centre of Kaleen.
What geological features are characteristic of the Kaleen area?
Kaleen sits on Silurian‑age Canberra Formation calcareous shale to the east and Ordovician‑age Pittman Formation greywacke to the west, separated by the Gungahlin Fault.