13 Brennan Street
13 Brennan Street, Hackett ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Nov 2014 | $870,000 | $677 |
| Sold | Aug 2007 | $430,000 | $334 |
Price per m² based on land size of 1285 m².
Key details
- Locality
- Hackett
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714886026
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/HACK/40/13
- Remoteness area
- Metro
- Property type
- House
- Land size
- 1285 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 the house at 13 Brennan Street have?
The home features five bedrooms and three bathrooms. It offers ample space for a large family or multi‑generational living.
What is the size of the land the property sits on?
The residence sits on a 1,285 m² block, providing generous outdoor area for gardens, recreation or future extensions.
How many parking spaces are available at the property?
Four parking spaces are provided on the premises, giving convenient vehicle accommodation for residents and guests.
How far is the house from Canberra’s central business district?
Hackett is situated about 4‑5 km north‑east of the Canberra CBD, making the location easily reachable by car or public transport.
What parks are located near 13 Brennan Street?
Calvert Park is roughly 0.8 km away, and Bill Pye Park is about 1.6 km distant, both offering green space for walking, picnics and recreation.
Is there a bus shelter or public transport stop close to the property?
The Officer Crescent bus shelter is situated approximately 1.5 km from the house, providing convenient access to local bus services.
What can you tell me about the geological setting of Hackett?
The suburb rests on calcareous shales of the Canberra Formation overlain by Quaternary alluvium, with the higher eastern side built on the lowest layer of the Ainslie Volcanics, a grey dacite with agglomerate and tuff.