16 Lapsley Street
16 Lapsley Street, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Nov 2021 | $876,000 | $1,908 |
| Sold | Aug 1997 | $124,500 | $271 |
| Sold | Nov 1996 | $38,000 | $82 |
Price per m² based on land size of 459 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714848597
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/51/8
- Remoteness area
- Metro
- Property type
- House
- Land size
- 459 m²
- Internal area
- 171 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 the house at 16 Lapsley Street have?
The property features four bedrooms and two bathrooms. It is a standalone house designed for family living.
What is the size of the land on which the house is built?
The home sits on a 459 m² block. This provides ample outdoor space for gardening or recreation.
What parking facilities are included with the property?
The residence offers two dedicated parking spaces. These are provided within the property's boundaries.
Which nature reserves or parks are located near 16 Lapsley Street?
Dunlop is bordered by the Dunlop Grasslands Nature Reserve as well as West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all part of the Ginninderra Catchment. The Boslem and Harte Park is also nearby, approximately 1.8 km away.
How far is the property from Canberra’s city centre?
The suburb of Dunlop lies about 11.6 km (roughly 7.2 mi) north‑west of Canberra’s central business district, making the city centre easily reachable by car.
What is the geological makeup of the Dunlop area?
Dunlop sits on Silurian‑age rocks, primarily Deakin Volcanics purple rhyodacite, with grey tuff from the Laidlaw Volcanics in the south‑west. The Deakin Fault runs along the north‑east edge, where green‑grey dacite and quartz‑andesite of the Hawkins Volcanics are uplifted.