24 Pomeroy Street
24 Pomeroy Street, Dunlop ACT 2615, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Jul 1994 | $72,000 | $39 |
Price per m² based on land size of 1805 m².
Key details
- Locality
- Dunlop
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714846330
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/DUNL/23/6
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1805 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
What is the size of the land associated with the property at 24 Pomeroy Street?
The property sits on a land parcel of approximately 1,805 m². This provides a generous block size for a single‑family house.
What type of residence is located on this parcel?
The listing describes the dwelling as a house, positioned on the 1,805 m² block.
Which natural reserves or water features are close to the property?
Within the suburb of Dunlop you’ll find the Dunlop Grasslands Nature Reserve, West Belconnen Ponds, Jarramlee Pond and Fassifern Pond, all part of the Ginninderra Catchment and located nearby.
How far is the nearest shopping centre from the property?
Kippax Fair Shopping Centre is approximately 2.4 km away, providing convenient access to retail and services.
What park is most nearby for recreational use?
The Boslem And Harte Park lies about 1.9 km from the house, offering green space and walking tracks.
Which federal and territory electorates include this address?
For Australian federal elections the property falls in the Division of Fenner, and for ACT Legislative Assembly elections it is part of the Ginninderra electorate.
What are the dominant geological features of the Dunlop area?
Dunlop’s geology is characterized by Silurian‑age rocks, largely Deakin Volcanics purple rhyodacite, with patches of grey tuff from the Laidlaw Volcanics and the Deakin Fault running along its north‑east edge.