A moraine is usually defined as a glaciated landform that is formed by the accumulation of sediments and the moving glaciers. It is comprised of well-sorted sediment particles, which are being shaped during its time of transportation.
There are three distinct types of moraines, namely-
Lateral moraine- These are found to be deposited along the sides of the glacier
Medial moraine- This type of moraines joins the two separate glaciers
Terminal moraine- This type of moraine is found at the end of the glacier. It is located at the furthest distance from the main glaciers.
The lowlands west of Australia´s eatern mountain range are drained by the Murray-Darling River system, with its main headwaters in the <em>Great Artesian Basin.</em>
