Dirk Hartog, 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
Most of Lake Macleod is normally dry, covering an area of 2,000 km2 (770 sq mi), 60 km2 (23 sq mi) of which is covered by perennial bodies of brine.[3]
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 salt beds 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.[4]
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[5]
^Johnson, Kaz (November 2011). "Lake MacLeod and the Northern Ponds"(PDF). Nedlands, WA: Rangelands Natural Resource Management. Retrieved 21 June 2023.
^Kavazos, Christopher (2016). Small-scale biogeographic patterns of benthic bacterial and ciliate communities in the saline ponds of Lake MacLeod, North-Western Australia (Thesis). doi:10.13140/RG.2.2.18785.10088.