11 Dorrit Black Crescent
11 Dorrit Black Crescent, Lyneham ACT 2602, Australia
Key details
- Locality
- Lyneham
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714892429
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/LYNE/97/6
- Remoteness area
- Metro
- Property type
- House
- Land size
- 496 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 type of property is located at 11 Dorrit Black Crescent?
It is a standalone house situated on a 496 m² land parcel. The property is located in the suburb of Lyneham, Canberra.
How large is the land associated with the house at 11 Dorrit Black Crescent?
The land size is 496 square metres. This provides ample space for a garden or outdoor entertaining area.
What nearby attractions or amenities are within walking distance of 11 Dorrit Black Crescent?
The Old Canberra Inn, a historic pub, is about 0.6 km away, and the National Hockey Centre is roughly 0.7 km distant. You can also enjoy Tilley's Café (≈1.3 km) and the ACT Clay Court International tennis event (≈0.2 km).
Which public transport options serve the area around 11 Dorrit Black Crescent?
Lyneham is serviced by several bus routes (R9, 30, 31, 50, 51) and light‑rail stations such as Swinden Street (≈1.2 km) and Dickson Interchange (≈1.5 km). The Sullivans Creek shared path also provides a convenient cycling route.
How would you describe the character of the Lyneham suburb where the property is located?
Lyneham features leafy streets, established gardens, and a mix of older 1960s homes with newer developments. The suburb offers easy access to nature parks, cultural venues, and a vibrant community atmosphere.
What geological features underlie the area around 11 Dorrit Black Crescent?
The site sits on Silurian calcareous shales from the Canberra Formation, overlain by Quaternary alluvium. In the north‑west of the suburb, Ordovician greywacke from the Pittman Formation is also present.