Snowdonia local case study of a glaciated environment: Flashcards
Location/characteristics:
- A glacial landscape in North Wales.
- Upland areas of snowdonia show many landforms.
- The area is no longer glaciated since the landforms formed.
- Landforms have been modified by periglacial processes and more recently fluvial action, weathering and human processes.
All the glacial landforms at Snowdonia:
U-shaped valley = Nant Francon.
Truncated spur - Y Gribin.
Arête = Y Gribin
Moriane = found around Llyn Idwal.
Kame and Esker = Pentir
Outwash plain = Conwy Bay.
Blockfields = Glyder Fach.
Corries and Tarns =
U- shaped valley name and facts about it …
- Nant Francon.
- Formed by a glacier that flowed in the direction towards the coast at Anglesey.
- River Ogwen flows in the valley now.
Corries and Tarns names and facts about it …
- Llyn Idwal = Tarn
- Cwm Idwal = Corries
Formed by tributary glaciers.
Truncated spur name and facts about it …
- Y Gribin
- Formed when interlocking spurs were truncated from the Nant Francon glacier.
Arête name and facts about it …
- Y Gribin.
Sharp ridge, caused by corries eroding either side of the ridge.
Moraine name and facts about it …
- Llyn Idwal.
Terminal moraine found at the mouth of the tarn.
Lateral moraine on the west side of the tarn
Kame and esker name and facts about it …
- Pentir.
- Formed by meltwater from the Nant Ffrancon glacier.
Outwash plain name and facts about it …
- Conwy Bay.
- Clear layer of glacial deposits.
Blockfields name and facts about it …
- Summit of Glyder Fach.
Caused by frost action weathering.