Lake Alexandrina is located east of
Encounter Bay and the
Fleurieu Peninsula within the contemporary South Australian government regions of the
Fleurieu and Kangaroo Island and
Murray Mallee regions. The
Murray River is the principal inflow to the lake. Additional tributaries include the
Bremer,
Angas, and
Finniss rivers, which drain the eastern slopes of the southern
Mount Lofty Ranges. The lake is shallow and contains a number of low-lying islands, particularly towards its southern extent.
Loveday Bay is an inlet located on the south-eastern margin of Lake Alexandrina, adjacent to the Tauwitchere Channel. The lake is connected by a narrow channel to the smaller
Lake Albert to the south-east. Lake Alexandrina drains towards the
Southern Ocean via the
Murray Mouth, located south-east of
Goolwa. Under conditions of low river discharge, the Murray Mouth is periodically closed by a sand bar, restricting exchange between the river system and the ocean. To regulate water levels and maintain freshwater conditions in the Lower Lakes system for irrigation, a series of
barrages, collectively known as the
Goolwa Barrages, were constructed across five channels between the mainland and islands near the Murray Mouth. Although the lake has historically experienced periods of connection with the ocean, hydrological studies indicate that freshwater conditions have predominated under typical river inflow regimes, with saline incursions largely restricted to episodic events associated with low discharge or marine high tides and storm surges. Where marine water enters the system, mixing with freshwater is generally limited, both vertically and laterally, depending on hydrodynamic conditions. A synthesis of research published in 2020 concluded that the Lower Lakes–Coorong–Murray Mouth system exhibited predominantly freshwater characteristics prior to European settlement, while acknowledging natural variability across time and space within the system.
Hindmarsh Island lies within the Lower Lakes system and is influenced by both riverine and marine processes due to its position between freshwater inflows and the estuarine reach of the Murray Mouth. It has been described in some sources as the largest island in the world to have freshwater on one side and saline water on the other, reflecting the contrasting hydrological conditions that can occur under varying river discharge and mouth openness. ==History==