23 Twamley Crescent
23 Twamley Crescent, Chisholm ACT 2905, Australia
Key details
- Locality
- Chisholm
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714915036
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/CHIS/501/33
- Remoteness area
- Metro
- Property type
- House
- Land size
- 892 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 23 Twamley Crescent have?
The property features four bedrooms, providing ample space for a family or home office.
What is the size of the land that the house sits on?
The house is set on a block of 892 m², offering a generous outdoor area for gardening, recreation, or future extensions.
What type of dwelling is located at 23 Twamley Crescent?
It is a detached house, typical of the low‑density residential layout in the Chisholm suburb.
What shopping and service amenities are close to the property?
The nearby Chisholm Group Centre on Halley and Benham Streets provides a Coles supermarket, tavern, restaurants, a GP, dentist, BP service station, fire station, rugby club, child‑care and other retail outlets.
Which public transport options serve the Chisholm area?
ACTION bus routes 74 and 75 run a circular service linking Chisholm with Tuggeranong Town Centre and Erindale Centre, while routes 76, 78 and the peak‑hour route 182 also connect the suburb to surrounding areas and the Monaro Highway.
What recreational facilities are available nearby?
Residents can enjoy the Chisholm District Playing Fields on Proctor Street, the Neighbourhood Oval on Alston Street, The Pines Tennis Club on Norris Street, and the walking tracks over Simpsons Hill, which is just about 0.6 km away.
What is the geological composition of the land under Chisholm?
The suburb sits on Deakin Volcanics, a Silurian volcanic formation featuring rhyolite throughout and rhyodacite in the eastern hill area, with rocks dating back roughly 414 million years and displaying a range of colours due to water alteration.