Before European settlement the lake was used by Aboriginal people as an important site for tortoise hunting, with campsites occupied for long periods. It is associated with the Waugal, a powerful and important water serpent in Noongarmythology that created rivers and lakes, and maintains the flow of waters to its resting places.
European settlement
The first non-Aboriginal settlement occurred in 1885, when William and Alfred Skeet were granted a 'Special Occupation' license for adjoining the lake, as well as licences to cut and sell timber. Farming around the lake began in 1893; much of the land was cleared, crops were trialled along with dairy and poultry farming. By 1898, the area around the lake had been set aside for a township with recommendations made for its subdivision. The Jandakot region started producing vegetables, apiary products and dairy produce for the Fremantle markets. From the 1920s agriculture gave way to sheep and cattle grazing, which continued through the next 50 years. During the 1940s the west side of the lake was heavily grazed by livestock, particularly during the drier summers when the lake's fringing vegetation served as supplementary fodder. As a result, the land on the west side of the lake lacks native understorey plants and is infested with introduced plants such as arum lilies. The lake was gazetted as an A-class Nature Reserve in 1957 for the protection of flora and fauna, as well as for recreation, particularly sailing. The population in the Forrestdale area increased rapidly in the late 1960s as the townsite blocks to the north-west of the lake were taken up. Since then the population has gradually increased to about 1350.
Forrestdale Lake is a shallow, brackish, seasonal lake with a large area of open water when full. It has extensive fringing sedgeland typical of the Swan Coastal Plain, and is a major breeding site, migration stop-over and semi-permanent drought refuge area for waterbirds. It usually dries out by mid-summer. The area to the north-east is suburban with houses only from the lake. Land to the west has been developed for agriculture or housing to about from the shoreline. There is a large area of natural open woodland on the eastern side.
Geology and hydrology
The lake lies on the eastern edge of the gently undulating Bassendean Dune System, which is formed mainly of leached grey-white siliceous sands. It is a deflation basin bordered by low sand ridges up to five metres high. On the north-eastern edge of the lake there is a rocky sandstone outcrop. The lake bed sediments are up to two metres thick and include clay, silt, peat, diatomite, marl and freshwater limestone. It also lies on the eastern margin of the Jandakot Mound, a region of elevated water table beneath the Swan Coastal Plain, where the mound intersects the Perth Groundwater Area. Water levels in the lake were much higher in the 1970s and 80s, and have been declining steadily since 1992. Groundwater levels have also decreased since records began in 1996 and are about below the levels of the 1970s and 1980s. The lake is now drying out earlier than in previous wetter years.
The use of pesticides to control chironomids is a potential threat to aquatic invertebrate and bird life; in 1984 about 220 shorebirds were killed at the lake as a result of such spraying. Increased groundwater abstraction may exacerbate already declining water levels. The area of bulrushes in the fringing vegetation has increased and threatens its ecological character by changing its floristics, reducing the amount of open water, and reducing the area of mudflat available to migratory shorebirds. Disturbance of waterbirds by humans and dogs may occur, especially in late summer and autumn when the lake is drying out. Increasing urbanisation of the catchment may change the water balance or increase the already high nutrient level.