1. LANDFORMS OF GLACIAL DEPOSITION
These slide-shows are all on the Geography blog if you wish to copy any notes from them; we will not be stopping in class for you to do this
LANDFORMS OF GLACIAL DEPOSITION
Materials carried by the glaciers are deposited in two main ways;
Glacial Deposits (unsorted) and
Fluvio-glacial deposits (sorted)
In your textbook, read the section about glacial deposition (page 99 – 104)

2. deposition It is angular in shape.
Moraine is the waste material worn away and collected by the ice.
It is angular in shape.
Glacial deposits are poorly sorted, ie all different sizes and rock types are mixed together.

3. deposition
See the moraine on the glacier surface.

4. deposition TYPES OF MORAINE
Lateral moraine is found on the sides of the glacier. Scree, from frost shattering, is an important source.
Ground moraine is found at the base (bottom) of the ice. It is also called till or boulder clay.
Supra-glacial
Englacial moraine is found inside the ice itself.
Medial moraine is found down the middle of the glacial surface and occurs when the inner lateral moraines of two glaciers join.
Terminal moraine is found in front of the snout of the glacier if it is stationary. It represents the maximum advance of the ice.

5. deposition 15

6. deposition
Terminal moraine
Snout of glacier

7. deposition
Erratics are large rocks that are completely different from the type of rocks on which they rest
ERRATICS
They were carried by the ice-sheet, sometimes for hundreds of kilometres
and then deposited.

8. deposition
Erratics like this are often found on the valley floor.

9. deposition
ESKER
Glacial streams are found under the ice.They are loaded with debris (sand and gravel) carried by the meltwater. As the ice retreats, the river deposits its load. The built-up river bed is called an Esker.
This river has all but dried up!

10. deposition
An esker is a steep-sided, long, winding ridge, made up of gravel and sand. Most are tree-covered.

11. deposition
DRUMLIN
Side view
Drumlins are smooth, rounded
mounds of ground moraine.
The steep (stoss) side faces the direction the ice
Moved from.
Drumlins often occur in swarms or groups on the valley floor.
Plan view

12. deposition
Here is a drumlin outside Buchlyvie.
Can you work out the ice direction?

13. deposition
Meltwater streams bringing outwash to be distributed across an outwash plain.
Note the braiding of the stream channels.

14. Can you name the Scottish examples we learned about in S Grade?
deposition
A KETTLEHOLE LAKE
Can you name the Scottish examples we learned about in S Grade?
LOCH MORLICH
There’s also the LAKE OF MENTEITH
depression formed when ice melts
depression filled with water to form kettle lake

15. deposition What is a kame terrace?
During the end stages of glaciation, a lake gathers at each side of the ice, filling with moraine.
GLACIER
Once the ice has melted, the debris has been lowered to the valley floor and created a terrace with a steep side and flattish top.
Kame terraces

16. deposition
This slide shows a set of kame terraces.

17. Identify the features shown on the diagram by matching
deposition
Identify the features shown on the diagram by matching
the numbers to the names given.
Esker / Terminal Moraine / Outwash Plain / Drumlin /
Till (Ground Moraine/Boulder Clay) / Kettlehole lake /
Outwash Sands and Gravels.

18. deposition
As you go through your revision, for each feature mentioned, look back through your textbooks and this presentation. You are looking for named examples of as many features as possible.
Remember that you will get marks in the exam and NAB’s for showing the skill of quoting places as examples from your notes!