7 St John Crescent
7 St John Crescent, Florey ACT 2615, Australia
Key details
- Locality
- Florey
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714887959
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- BELC/FLOR/174/11
- Remoteness area
- Metro
- Property type
- House
- Land size
- 712 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 on which the house at 7 St John Crescent is built?
The property sits on a 712 m² land parcel. This provides ample space for a detached house and outdoor areas.
How close is the property to the nearest beach?
Yerra Beach is the closest, located about 0.4 km away. Other nearby beaches such as Bargang Beach and Dulwa Beach are within 0.6–0.7 km.
What public transport options are available in Florey?
Florey is served by three ACTION bus routes – Route 2, Route 3 and Route 40 – providing connections to the wider Canberra network.
Have there been any recent environmental improvements near the property?
In 2018 the ACT Healthy Waterways Project restored parts of a concrete drainage channel along Tattersall Crescent, returning it to a more natural creek‑like state to help slow and clean stormwater flowing into Ginninderra Creek.
What community facilities are within walking distance of 7 St John Crescent?
The Florey shopping centre is situated on the corner of Kesteven Street and Ratcliffe Crescent, and the Hindu Temple and Cultural Centre on Ratcliffe Crescent are also nearby, offering cultural and daily‑shopping amenities within the suburb.
How far is Lake Ginninderra from the house?
Lake Ginninderra lies approximately 1.2 km from the property, making it a short drive or bike ride away for recreation.
What type of geology underlies the Florey area?
Florey sits on Silurian‑age rocks, including green‑grey dacite, quartz andesite, various rhyodacites and rhyolites, as well as calcareous shale, with the Deakin Fault running through the region.