35 Nina Jones Crescent
35 Nina Jones 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.
- GAACT714899028
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- TUGG/CHIS/10/22/1
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1153 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 for the house at 35 Nina Jones Crescent?
The property sits on a 1,153 m² block, providing ample space for outdoor activities and potential landscaping.
How far is the property from Simpsons Hill and what can be done there?
Simpsons Hill is about 0.8 km away; it offers wilderness walking tracks popular for dog walks and nature walks.
What public transport options serve the area around 35 Nina Jones Crescent?
Several ACTION bus routes serve Chisholm, including routes 74/75 (a circular service to Tuggeranong Town Centre), routes 76 and 78, and the peak‑hour route 182 that runs via the Monaro Highway.
What shopping and service amenities are nearby?
The Chisholm Group Centre on Halley and Benham Streets, within a few kilometres, provides a Coles supermarket, tavern, restaurants, a GP, dentist, BP service station, fire station and other businesses.
Which recreational facilities are close to the property?
The suburb features the Chisholm District Playing Fields on Proctor Street, the Chisholm Neighbourhood Oval on Alston Street, and The Pines Tennis Club on Norris Street, all located roughly 1–2 km from the house.
Under which federal and ACT electoral divisions does the property fall?
It lies in the federal electorate of Bean, represented by David Smith, and in the ACT Legislative Assembly electorate of Brindabella.
What is the geological composition of the land beneath Chisholm?
The suburb sits on Silurian‑age volcanic rocks of the Deakin Volcanics, primarily rhyolite with rhyodacite to the east, dating back about 414 million years.