Fraser Avenue aerial viewKings Park sits upon the tableland area of the Mt Eliza escarpment, which rises steeply from the Swan River to a high point in the landscape of 65 m and is visible from the city foreshore and surrounding suburbs. Views from the escarpment overlook Perth City, the Swan River and Darling Scarp in the distance. Geologically it is within the Spearwood Dune System with soils of the Karrakatta Soil association.

Over time, leaching of the calcareous sands has led to the formation of limestone at greater depths. This is demonstrated by the limestone cliffs exposed above Mounts Bay Road. As a result of past weathering, Kings Park slopes from high areas in the south-east to low lying areas in the south-west. The limestone cliffs have been exposed as the Swan River receded, and are a significant landform of the bushland.

The soils can be divided into two main types: medium size, calcareous sands; and shallow sands with exposed limestone. Apart from sand varying in pH, degree of leaching and grain size, there are areas of sandy loams. The underlying sand loam sheets, with perched water tables (for some months of the year) are important as they coincide with more vigorous vegetation cover.

These soils support three major plant communities which provide for a diverse array of flora, fauna and fungi.

Saw Avenue access disruption

Visitor disruptions will occur in the Saw Avenue Picnic Area from Monday 25 March 2019 due to toilet facilities upgrade works.

Visitor reminder

Under BGPA Regulations, an infringement may be issued if the driver of a vehicle does not remain within Kings Park's boundaries.

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Botanic Gardens Day

What is a botanic garden we hear you ask? The answer is that botanic gardens are much more than ‘just a pretty face’.

Grow perfect pink everlastings

Did you know May and June are the perfect months to sow your everlasting seeds to ensure they bloom in spring?

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