42 Frater Crescent
42 Frater 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.
- GAACT714886974
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/LYNE/81/7
- Remoteness area
- Metro
- Property type
- House
- Land size
- 546 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 dwelling is located at 42 Frater Crescent and how large is its land parcel?
The property is a standalone house situated on a 546 m² block of land. It offers the space typical of single‑family homes in Lyneham.
Which sporting and recreational venues are closest to 42 Frater Crescent?
The National Hockey Centre is about 1.1 km away and the Canberra Racecourse is roughly 1.6 km distant. Nearby also are the ACT Clay Court International tennis tournament site (0.7 km) and the Old Canberra Inn, a historic hotel (1.0 km).
How can residents of 42 Frater Crescent access public transport?
The Swinden Street light‑rail stop is approximately 1.4 km from the property, providing convenient metro service. In addition, several bus routes (R9, 30, 31, 50, 51) serve the Lyneham area.
What is the historical background of the suburb where this house is located?
Lyneham was gazetted in 1928 but development began in 1958, with streets named after artists and early Canberra figures. The suburb has evolved from 1950s‑era homes to a mix of modern townhouses and renovated properties, retaining leafy streets and established gardens.
What natural attractions are found near 42 Frater Crescent?
Lyneham offers bushland nature parks and a scenic wetland adjacent to Sullivans Creek, opened to the public in 2012 and frequented by wood ducks. These green spaces provide easy walking and wildlife‑watching opportunities close to the home.
What geological features underlie the area around 42 Frater Crescent?
The site sits on Silurian calcareous shales of the Canberra Formation, overlain by Quaternary alluvium, which was historically referred to as the "Limestone Plains". In the north‑west of the suburb, Ordovician greywacke from the Pittman Formation is also present.