Presentation is loading. Please wait.

Presentation is loading. Please wait.

Glacial Processes and Landforms

Similar presentations


Presentation on theme: "Glacial Processes and Landforms"— Presentation transcript:

1 Glacial Processes and Landforms

2 What do you know about the Ice Age?

3 What evidence is left of the Ice Age?

4 ICE AGE Definition a period of time with low global temperatures and extensive glaciation.

5 What is a glacier? How do glaciers form?

6 What is a glacier? A glacier is simply the existence of year-round ice on the landscape. (A huge mass of ice slowly flowing over a land mass) There are two broad types: continental and alpine. How do glaciers form? Glaciers form whenever snowfall exceeds snowmelt year after year. The snow accumulates incrementally, pressure increases, and it is changed into névé and then ice by this pressure.

7 Why are glaciers important?
Fresh water from glaciers

8 Maximum Extent of Pleistocene Glaciation - 1/3 of land surface
Most recent glacial maximum peaked 18,000 years ago and is considered to have ended 10,000 years ago

9 Current Extent of Glaciation -
about 10% of land surface

10 Where da’ glaciers at?

11 Have you ever seen a glacier???
Perfect for surfing, right!?

12 Vocab time!

13 Where are the zones??? Franz Joseph Glacier and Outwash Plain, New Zealand

14 Erosion by Glaciers volume and speed determines amount of erosion.
erodes slightly more effectively than water. plucking and abrasion (rock-tipped blade). polishing and striations. Continental glaciers remove all soil, plants, and small hills. Alpine glaciers change V-shaped valleys to U-shaped.

15 What happens when glaciers melt!?

16 What do these words mean!?
Vocab time (again!)

17 Where is the evidence!

18 What glacial evidence do you see here?

19 What about here?

20 Transportation by Glaciers
will move material of all sizes, from glacial flour to massive boulders. Slow transport. Water in, on, and under glaciers (pluvial processes) moves much sediment as well.

21

22 Bro, let’s go inside a glacier!!! Video – “Inside a Glacier”
Why am I friends with him… Bro, let’s go inside a glacier!!! Video – “Inside a Glacier”

23 Deposition by Glaciers
Drift is any material deposited by glaciers or their meltwater. Till is that unsorted material that is deposited directly by ice. *Moraines are linear features deposited at the bottom or along the sides of glaciers. Glacial erratics are enormous boulders transported and deposited by glaciers, often far from their source region.

24 Beware!! Glacial erratics on the loose!

25 Alpine Glaciers – using your vocab words!
UV

26 Vocab time (again!!) Then, let’s go back…

27

28

29

30

31

32

33 Moraines

34 The 3 moraine sisters (disguised vocab)

35

36 Identify the moraines!

37 Finger Lakes Region, New York

38 Continental Glaciers or Ice Sheets
only two true ice sheets exist today: Greenland and Antarctica where they meet the sea they can form ice sheets. vary in thickness from hundreds of feet to two miles deep! scour away all soil and vegetation and dramatically reshape the landscape and ecology of large regions. much change occurs in the periglacial environment. (periglacial = around the glacier) How many are there? Ellesmere Island, Canada

39 Continental Glaciers or Ice Sheets
/ Last little bit of vocab! (and there was much rejoicing)

40 Continental Glaciers or Ice Sheets

41

42

43

44

45

46 Fjords


Download ppt "Glacial Processes and Landforms"

Similar presentations


Ads by Google