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Material deposited by glaciers is collectively termed GLACIAL DRIFT –  It can be sub-categorised into: DIRECT DEPOSITION TILL  - Glacial deposits, unstratified and unsorted material (boulder clay) – large fragments of rock of all sizes and shapes randomly mixed together. Can be divided into: 1. lodgement till –  deposited at base of glacier due to basal melting – material is smeared onto the underlying rock due to the pressure of the ice as it continues to move  2.   ablation till –  material deposited as the ice melts away (coarser than lodgement till 2. INDIRECT DEPOSITION  a. FLUVIOGLACIAL  – picks up load once carried by ice (often then carried beyond limits of glacier – sorted and stratified by the action of water  b. ICE – CONTACT STRATIFIED DRIFT  – partly sorted by water – roughly stratified – deposited in vicinity of melting ice. GLACIAL DEPOSITION
Features of Glacial Deposition: Till Deposits ,[object Object],[object Object],[object Object],[object Object]
A DRUMLIN
DRUMLINS ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
A Drumlin Field – also known as a Drumlin Swarm – typical “Basket of Eggs” topography
Western Alberta, Canade ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Examples of Drumlins : Hellifield, Ribblesdale – North Yorkshire  – Swarms 40m high, 50-500m long – may be the result of ice sheets coming down from the Lake District, overloaded – change of gradient on the lowlands may have caused the ice to deposit the drumlins here. Other examples: New York State (USA) –  largest drumlin field – 10,000 drumlins!   Eden Valley - Cumbria
Stoss End Lee Slope Direction of Ice Flow
Lateral Moraine ,[object Object],[object Object],MORAINES
Medial Moraine ,[object Object],[object Object],[object Object]
Terminal Moraine ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Recessional Moraine ,[object Object],[object Object],[object Object],[object Object]
Push Moraine ,[object Object],[object Object]
ERRATICS ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
TILL PLAINS ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Reference: All photographs used for educational use only – sourced from google images.

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Glacial Deposition A2

  • 1. Material deposited by glaciers is collectively termed GLACIAL DRIFT – It can be sub-categorised into: DIRECT DEPOSITION TILL - Glacial deposits, unstratified and unsorted material (boulder clay) – large fragments of rock of all sizes and shapes randomly mixed together. Can be divided into: 1. lodgement till – deposited at base of glacier due to basal melting – material is smeared onto the underlying rock due to the pressure of the ice as it continues to move 2. ablation till – material deposited as the ice melts away (coarser than lodgement till 2. INDIRECT DEPOSITION a. FLUVIOGLACIAL – picks up load once carried by ice (often then carried beyond limits of glacier – sorted and stratified by the action of water b. ICE – CONTACT STRATIFIED DRIFT – partly sorted by water – roughly stratified – deposited in vicinity of melting ice. GLACIAL DEPOSITION
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  • 5. A Drumlin Field – also known as a Drumlin Swarm – typical “Basket of Eggs” topography
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  • 7. Stoss End Lee Slope Direction of Ice Flow
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