57 Holmes Crescent
57 Holmes Crescent, Campbell ACT 2612, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Aug 2010 | $1,005,000 | $1,066 |
| Sold | May 2000 | $353,000 | $374 |
| Sold | Jan 1995 | $250,000 | $265 |
Price per m² based on land size of 942 m².
Key details
- Locality
- Campbell
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714881362
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/CAMP/57/17
- Remoteness area
- Metro
- Property type
- House
- Land size
- 942 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 and bathrooms does 57 Holmes Crescent have?
The house features four bedrooms and two bathrooms, providing ample space for a family.
What is the size of the land that the property sits on?
The residence sits on a 942 m² block, offering a generous garden and outdoor area.
Is there a garage or dedicated parking with the house?
Yes, the property includes one garage, providing secure off‑street parking.
How close is the nearest park to the home?
Victoria Cross Park is only about 0.6 km away, while George Cross Park is roughly 1 km from the property, both within easy walking distance.
What major educational or defence institutions are nearby?
UNSW Canberra is approximately 0.6 km away, and the Australian Defence Force Academy is about 0.7 km from the house, making them very accessible.
What does the demographic profile of Campbell look like?
Campbell had a population of 6,564 in the 2021 census; around 70% were born in Australia, 78% speak only English at home, and the most common religions are No Religion, Catholic and Anglican.
What geological features are characteristic of the Campbell area?
The suburb sits on the Ainslie Volcanics, primarily grey dacite with layers of quartz andesite and cream rhyolite formed in the Silurian period, underlain in some parts by Tertiary pebbly gravels.