16 Tanderra Crescent
16 Tanderra Crescent, Ngunnawal ACT 2913, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Oct 1996 | $80,000 | $45 |
Price per m² based on land size of 1755 m².
Key details
- Locality
- Ngunnawal
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714910368
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/NGUN/164/14
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1755 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 does the house at 16 Tanderra Crescent have?
The property offers five bedrooms, providing ample space for a large family or guests.
What is the size of the land on which the house is built?
The home sits on a 1,755 m² block, giving plenty of room for outdoor activities and landscaping.
How far is the property from the Gungahlin Town Centre?
It is located about 4 km from the Gungahlin Town Centre, a short drive to shops, services and dining.
What parks or recreational areas are close to the house?
Within 0.5 km you’ll find Ginninderra Park and the Gungahlin Enclosed Oval, and Yerrabi Pond is just 0.8 km away, offering walking and leisure options.
Is there easy access to public transport nearby?
The Gungahlin Place light‑rail stop is roughly 1.2 km from the property, providing convenient rail connections to the wider ACT.
What are some local attractions or community facilities near 16 Tanderra Crescent?
The Gold Creek Homestead and the Marketplace Gungahlin shopping centre are each about 1.2 km away, while the Gungahlin Community Council is within 0.9 km, offering a range of local services.
What geological features characterize the Ngunnawal area?
Ngunnawal sits on the Canberra Formation with slaty shale and mudstone, and contains pockets of dacite, quartz‑andesite, and tuff exposures that have been studied for their Silurian‑age rock structures.