75 Bimberi Crescent
75 Bimberi Crescent, Palmerston ACT 2913, Australia
Key details
- Locality
- Palmerston
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714919083
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- GUNG/PALM/104/2/8
- Remoteness area
- Metro
- Property type
- Unit
- Land size
- 4584 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 75 Bimberi Crescent?
The address is a stand‑alone unit. It is part of the residential mix of single homes and duplexes that characterise Palmerston.
How many bedrooms does the unit at 75 Bimberi Crescent have?
The unit comprises two bedrooms, making it suitable for small families or couples seeking a low‑maintenance home.
What is the size of the land parcel on which the unit sits?
The property sits on a 4,584 m² land parcel, providing a generous outdoor space relative to typical units in the area.
Which public transport routes serve the Palmerston suburb where the unit is located?
ACTION bus routes 21, 22, 23 and 24 travel along Kosciuszko Avenue and other streets in Palmerston, connecting the suburb with Gungahlin Town Centre, Franklin and Nicholls.
What parks and recreational areas are close to 75 Bimberi Crescent?
Within about 2 km you’ll find George Kemp Park (≈1.1 km), Girrawah Park (≈1.5 km), Ginninderra Park (≈1.5 km), Gungahlin Hill (≈1.6 km) and the Gungahlin Enclosed Oval (≈1.8 km), all offering open space and walking paths.
What geological formation underlies the Palmerston area?
Palmerston sits on the late middle Silurian Canberra Formation, primarily composed of slaty shale and mudstone, with notable ashstone exposures that form distinctive ear‑of‑corn‑shaped outcrops.
Are there any notable geological faults near the property?
Yes, the Winslade Fault approaches from the south and joins a long fault along the east side of Ginninderra Creek, while the Gungahlin Fault also runs parallel to the local folds, forming the eastern limit of the ashstone band.