1. Ribbon/Finger Lakes: Lake caused by glaciers carving deep grooves in less resistant rock
Fjords: Glacial valleys/ troughs filled with ocean water
Kettle Lakes: Depression formed after an isolated block of ice melts.

2. Erosional Features: Finger Lakes

3. Erosional Features: Fjords

4. Erosional Features: Kettle Lakes

6. Depositional Features
Lateral Moraine: Till collected on valley sides by rock falls and plucking off valley walls.
Medial Moraine: Formed by meeting of lateral moraines as two glaciers meet
Terminal/End Moraine: Deposited at the furthest point of glacial advance.

7. Depositional Features: Moraines

10. An esker is a snake-shaped deposit of till, formed when running water flows through paths along the bottom of a glacier
Crevasses are deep cracks in the surface of a glacier. They can be extremely dangerous to anyone walking on a glacier
An icefall is when huge blocks of ice fall off the sides of a glacier

12. Features of Continental Glaciers
Outwash Plains/ Lacustrine Deposits: Sand and other sediment deposited by glacial melting.
Erratics are large boulders that are left in odd locations when glaciers melt
A roche moutonee is formed when a glacier moves over outcrops of bedrock. The side facing the glacier is polished smooth, while the other side is jagged from plucking

13. Depositional Features: Outwash Plains

14. Drumlin: Hill made up of deposits from glaciers movement.
Continental glaciers produce many similar features to alpine glacier, such as U-shaped valleys and hanging valleys

15. Benefits of glaciers
Glaciers left behind much of our fresh water, in the form of lakes
Glaciers created the wide u-shaped valleys in which many people live (especially in BC)
Many gravel and sand deposits come from glacial drift
Glacial deposits provide rich soil in many areas