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Published byAmelia Kennedy
Modified over 4 years ago
Post-Glacial Modifications K.I. 3 b
Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran destroying Yungay and leaving deposits in a U Shaped Valley
Maen Llia – facing south – Post Glacial south facing Valley in Brecon Beacons
Llia Valley – and Fluvial V notch cut since end of Ice Age
Post Glacial scree And weathering of scree - Llyn Cau, Cader Idris
Cwm Amarch entering Tal-Y-Llyn (post Glacial Alluvial Fan)
The site of Keswick – post glacial alluvial deposition.
Earth Movement modifications…. Hveragerdi, Southern Iceland
Jura – Scottish west Coast – waterfall from raised cliff. Rejuvenation of river
Geiranger fjord and ferry - Norway
Dalmatian Type drowned coast British Columbia Canada
The Influence of Geology in the Development of Glacial Landforms.
Key Idea 1: Different forces shaping landforms.
Corrie, cirque, cwm – hollow where a glacier formed
High Energy Events And longer intervening periods of relative stability How do they influence the evolution of glaciated landscapes?
Glaciation Learning Intentions
Earth’s Surface Chapter 3 Erosion and Deposition
Big Idea 6: Earth Structures
Sealevel Changes and Landforms Miss B How does Sea level Change? There are two types of change 1- Eustatic - Global rise in sea water levels related.
Changes in Relative Sea Levels And their associated landforms.
Chapter 3 Section 2 Pages 72-81
It is a from a hill called Y Gyrn above the Storey Arms. The mountain is Fan Fawr. Here we find a watershed. To the south water runs down into the Taff.
Glaciation in Snowdonia - Some Post-Glacial Changes to the Landscape.
Landforms and Landscapes of Mountain Glaciers. Objectives Examine the current distribution of mountain glaciers and to comment on the Late Cenozoic extent.
LITHOSPHERE GLACIATION 1 Glaciation 2 Selkirk High School.
Chapter 11 Rivers & Groundwater.
Weathering, Erosion and Deposition
Erosion and Deposition
Unit 1 Lesson CHOICE 1CHOICE 2CHOICE 3 CHOICE CHOICE
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