CASE STUDY-CAIRNGORMS, SCOTLAND Flashcards
1
Q
talus slopes
A
freeze thaw on glacially steepened rock faces=talus slopes of rockfall debris (screes) between 10-20,000 years ago=higher rates of accumulation compared to now
2
Q
blockfields
A
freeze thaw weathering breaks up exposed ground (well jointed). common on the summit of Ben Macdui
3
Q
tors
A
small ,rock hills (made of granite) produced by different weathering and erosion. hydrolosis, mass movement and freeze thaw creates tors