, a Dutchman, made the first authenticated landing by a European along this coastline in 1616. Early explorers recorded phenomenal tidal ranges along this coast.
Description
Climatically, this part of Western Australia is greatly influenced by the north-flowing Western Australian Current that brings cool water northward from Antarctica, which is not conducive to producing inland precipitation. This cool offshore current, coupled with a very flat coastal plain, contributes to the near-desert-like conditions along the coastal region as evidenced by the brown landscape around the lake and the highly reflective saltbeds within the lake. The low point in the lake appears to be near the northern end where the light blues indicate some standing water. Close inspection of the image discloses very faint lines at the southernmost end of Lake Macleod where large evaporation beds are used for the production of high-quality salt and gypsum.
Environment
The lake is recognised as a DIWA wetland as it is an outstanding example of a major lake situated on the coast that is periodically inundated by freshwater
Birds
Some of the permanent ponds in the north-western part of the lake have been identified by BirdLife International as an Important Bird Area because they support fairy terns, over 1% of the world populations of red-necked stints, curlew sandpipers, banded stilts, red-necked avocets and red-capped plovers, as well as a population of dusky gerygones. The northern ponds consist of intermittently flooded, brackish to hypersaline mudflats surrounding saline springs and permanent saline channels and lagoons. Large numbers of red knots, Australian pelicans, little black cormorants, black-tailed godwits and black-winged stilts have been recorded. A substantial population of canary white-eyes is present.A review of the importance of the lake for shorebirds showed that it hosted significant populations of 10 species of which red knot, red-necked stint and curlew sandpiper occurred in internationally significant numbers.
