19 Myall Street
19 Myall Street, O'connor ACT 2602, Australia
Key details
- Locality
- O'connor
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714899357
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/OCON/29/8
- Remoteness area
- Metro
- Property type
- House
- Land size
- 791 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 19 Myall Street?
19 Myall Street is a detached house. It is part of the leafy, single‑dwelling character of the O'Connor suburb.
How large is the land parcel for the property?
The house sits on a 791 m² block, providing ample garden space typical of homes in O'Connor.
How would you describe the suburb of O'Connor where the property is situated?
O'Connor is an affluent Canberra suburb known for its leafy, heritage‑listed streets and a mix of historic homes and natural reserves. The area features a small shopping centre, community clubs, and a strong sense of heritage.
Are there any heritage‑listed sites close to 19 Myall Street?
Yes, the heritage‑listed Tocumwal houses are approximately 0.7 km away, and the Scout Hall, another heritage site, is also within the suburb.
What shopping and dining facilities are available nearby?
The O'Connor small shopping centre offers a pub/bar, grocery store, a couple of restaurants, a pharmacy, a hairdresser, a bicycle shop, and a florist, all within easy walking distance of the property.
What natural or recreational areas can residents enjoy close to the property?
Residents can access the O'Connor Ridge, part of Canberra Nature Park, for bush walking and mountain biking, and Jandura Park is about 1 km away, providing open space for leisure activities.
What are the main geological features of the O'Connor area?
The suburb sits on calcareous shales from the Canberra Formation overlain by Quaternary alluvium, with higher western parts featuring Black Mountain Sandstone and the northern ridge containing Ordovician Greywacke.