74 Wakefield Avenue
74 Wakefield Avenue, Ainslie ACT 2602, Australia
Key details
- Locality
- Ainslie
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714871416
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/AINS/30/21
- Remoteness area
- Metro
- Property type
- House
- Land size
- 965 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 residence is located at 74 Wakefield Avenue and how large is its land?
The property is a standalone house situated on a 965 m² block of land.
How far is the house from the nature trails of Mount Ainslie?
Mount Ainslie is within walking distance of the suburb, offering an easy paved walk or a direct “goat track” up the hill from the area.
Which parks are located close to 74 Wakefield Avenue?
Nearby green spaces include Rugby Park (about 0.5 km away), Keith Tournier Enclosed Oval (≈0.5 km), Corroboree Park (≈0.7 km) and Bill Pye Park (≈0.8 km).
What public transport options are available near the property?
The residence is close to several bus shelters, Cowper Street (≈0.2 km), Campbell Street (≈0.4 km) and Officer Crescent (≈0.9 km), and the Macarthur Avenue light‑rail station is about 1 km away.
What local amenities can residents walk to from 74 Wakefield Avenue?
The suburb’s central shopping strip is within walking distance and offers an IGA supermarket, a café, restaurants, a liquor store, a pharmacy, a laundrette, a Pilates studio and a newsagent.
How would you describe the character and atmosphere of the Ainslie neighbourhood?
Ainslie features leafy streets, mature deciduous trees and a village‑like atmosphere, with many early‑twentieth‑century heritage‑listed houses and a mix of modest and more recent infill developments.
What geological formations underlie the Ainslie area?
The ground consists of calcareous shales from the Silurian‑age Canberra Formation, overlain by Quaternary alluvium, reflecting the historic “Limestone Plains” of the region.