Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing...
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![Page 1: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/1.jpg)
Post-Glacial Modifications
K.I. 3 b
![Page 2: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/2.jpg)
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
![Page 3: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/3.jpg)
Maen Llia – facing south – Post Glacial south facing Valley in Brecon Beacons
![Page 4: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/4.jpg)
Llia Valley – and Fluvial ‘V’ notch cut since end of Ice Age
![Page 5: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/5.jpg)
Post Glacial scree
And weathering of scree
- Llyn Cau, Cader Idris
![Page 6: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/6.jpg)
Cwm Amarch entering Tal-Y-Llyn (post Glacial Alluvial Fan)
![Page 7: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/7.jpg)
The site of Keswick – post glacial alluvial deposition.
![Page 8: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/8.jpg)
Earth Movement modifications….
Hveragerdi, Southern Iceland
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Jura – Scottish west Coast – waterfall from raised cliff.Rejuvenation of river
![Page 10: Post-Glacial Modifications K.I. 3 b. Modification by a High energy Event within the existing geomorphological environment Alluvione from Mt. Huascaran.](https://reader036.fdocuments.us/reader036/viewer/2022070305/5515c139550346486b8b63e3/html5/thumbnails/10.jpg)
Geiranger fjord and ferry - Norway
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Dalmatian Type drowned coast
British Columbia Canada