1. Moraines: These are ridges of unsorted rock debris (till) deposited by glaciers. There are different types of moraines:

* Terminal Moraine: Marks the furthest extent of a glacier.

* Lateral Moraine: Forms along the sides of a glacier.

* Medial Moraine: Forms in the middle of a glacier, where two lateral moraines merge.

* Recessional Moraine: Forms as a glacier retreats, leaving behind a series of moraines.

2. Outwash Plain: This is a flat, gently sloping plain composed of sand and gravel deposited by meltwater streams flowing from a glacier. Outwash plains are often characterized by braided stream channels and kettle lakes.

3. Drumlins: These are elongated, oval-shaped hills composed of till. They are typically oriented parallel to the direction of ice flow. Drumlins form when a glacier flows over a pre-existing deposit of till.

4. Eskers: These are winding ridges of sand and gravel deposited by meltwater streams that flowed within or beneath a glacier. Eskers can be quite long and often form sinuous patterns on the landscape.

These are just a few examples of glacial deposition features. There are many others, including kames, kettle holes, and glacial erratics.