Geology Geologically, Mount Eliza is part of the Spearwood Dunal system which were formed during the
Pleistocene glacial and
interglacial periods around 40,000 years ago. This system is identifiable by its yellow brown sands over
Tamala Limestone. Mount Eliza's soil is of the Karrakatta soil association, formed from calcareous beach sand containing 50–70%
calcium carbonate. The leaching of this carbonate over time has created the limestone bases which have been exposed as the Swan River has receded. A drilling survey in 1971 found that both the escarpment and tableland area had a diverse nature of sand grain, depth and overall fertility. This diversity of sand sheets is explained by the operation of
Aeolian deposition and erosion over extended periods of time. Underlying sand loam sheets, with perched water tables are considered highly important for vegetation growth and subsequent stabilisation. The
Botanic Gardens and Parks Authority manages risk associated with geotechnical instability, and between 1995 and 2020 has made two geotechnical inspections with no major concerns.
Flora Within Mount Eliza's tableland and escarpment area there are 326 species of local native plants growing, which represents close to 15% of the native flora in the Perth region. Within this, three major plant communities are supported; limestone health land,
banksia woodland and low moist areas. Prior to European settlement, the bushland would have been dominated by tall Tuart (eucalyptus gomphocephala), Jarrah (Eucalyptus marginata) and Marri (Corymbia calophylla) with Banksia species sub-dominating. Today the bushland is dominated by Banksia species, and the original ecosystem of tall open forest of tuart-jarrah-marri is likely collapsing to be replaced by Banksia and low woodlands. This is a natural sequence, yet some say it has been accelerated by disturbance from settlement.
Fauna Kings Park has a wide variety of local birds and invertebrates, with over seventy bird species, twenty reptile species and hundreds of different invertebrates within the bushland of Mount Eliza. Kings Park and the Mount Eliza escarpment has been subject to various long-term studies on urban avifauna. A study in 1996 found that the
Brown Honeyeater and
Red Wattlebird were the two most abundant birds in the Mount Eliza escarpment. In addition, the study found that there was a higher abundance of birds, specifically nectivores during the spring season, likely due to the flowering plants. Despite this increase, there was a relatively small amount of nectivores in the Mount Eliza escarpment compared to other regions studied. Furthermore, a study in 2013 found that the three most abundant species in the bushland surrounding Mount Eliza were the Brown Honeyeater,
Singing Honeyeater and Red Wattlebird. Invertebrates of significant conservation value such as the Scarp Snail and the
trapdoor spider are confined to the Mount Eliza escarpment of Kings Park. == History ==