❄️ glaciation sg3a Flashcards
which physical factors influence the formation of landforms within the landscape system (5)
- geology
- aspect
- latitude
- altitude
- relief
what are the 3 different geological areas in lake district
- skiddaw group
- borrowdale volcanic district
- windermere group
characteristics of skiddaw group
- rounded mountains
- slates
- not resistant to weathering/erosion
- metamorphic rocks
characteristics of borrowdale of volcanic group
- igneous rock
- resistant to weathering & erosion
- dense interlocking rock structure with joints
- rugged topography (125 corries as lots of places for them to form)
characteristics of windermere group
- sedimentary rocks
- least resistant to erosion
- gentle foothills
how does altitude influence formation of landforms
high altitude (up to almost 1000m above sea level) = colder so glaciers can form
how does aspect affect formation of landforms
less sun on north/east sides of mountains = more accumulation = more diagnesis = larger mass of snow = more potential energy = more rotational movement & more rotational slip so corrie glaciers can form
examples of corries in lake district and description
- nethermost cove
- red tarn: 716m above sea level, backwall is 216m tall, 500m^2, north east orinetated
example of arête in lake district and description
striding edge: 1.5km long
example of hanging valley in lake district and description
glenridding beck
- 5km long
- 560m below red tarn
example of ribbon lake in lake district and description
ullswater: 11km long, 900m wide
example of glacial trough in lake district and description
patterdale: 13km long, 2km wide, 200-300m tall (sides)
example of peak in lake district and description
helvellyn fell: 950m above sea level
example of roche moutonnee in lake district and description
norfolk island: in ullswater, 1000m^2
examples of moraine in lake district and description
- hummocky moraine: glenridding beck, retreating corrie glacier = mounds of toll left by ice when it melts
- end moraine: red yarn corrie lip created when erosion decreases
example of drumlins in lake district and description
eden vale: 308 drumlins, glacier thins in zone of ablation = less competency so drumlins created
example of erratics in lake district and description
allonby: north west coast of cumbria
how are hanging valleys and glacial troughs interrelated
tributary glacier in hanging valley added mass to valley glacier = more potential energy = more kinetic energy = more erosion of trough
how are erosional landforms & depositions landorms interrelated
plucking & weathering steepens backwall of a corrie but also created subglacial debris which is deposited in zone of ablation eg moraine
short term changes to glacial landforms in lake district
mass movement
- rockfall eg creating scree slopes on backwall of a corrie or on a drumlin
medium term changes to glacial landforms in lake district
FTW
- water enters cracks, seasonal temp change is needed for it to freeze & melt repeatedly
biological weathering
- plants grow in warmer periods = carbonation/roots cracking rocks
long term changes to glacial landforms in lake district
glacial erosion:
- during ice age corrie glacier forms & erosional processes shape the corrie
glacial deposition:
- during ice age subglacial sediment deformation led to drumlins forming