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GeogOnline... Glacial Deposition Processes
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Geographers classify glacial sediment according to its mode of deposition. The collective name for all the sediments and debris deposited under glacial conditions is Glacial Drift. Sediments that were deposited by melting ice or by glacial streams are called Fluvio-glacial. Debris deposited directly by the glacier, such as Moraine and intra-glacial material dropped 'in situ' by retreating ice, is known as Till See photo: Till: Sierra Nevada, California.
		So there are not really a list of processes like abrasion and plucking that occur for glacial erosion. The photo shows the Saimaa drainage region which covers most of the southern part of eastern Finland, a region about the size of Belgium. In places, there is more shoreline here per unit of area than anywhere else in the world, the total length being nearly 15,000 km. The number of islands in the region is 14,000 Saimaa was created by the continental ice sheet in the Ice Age. Ice more than a kilometre thick then covered the entire area; when it melted, Saimaa gradually emerged through various stages as a freshwater basin separate from the sea and about 76 metres above sea level. Towards the end of the Ice Age, landscape features were created by meltwater gravel deposits.