e8ce8054_KS2_TT___Earth_Science_On_Site__Observations_teaching_points
[Interpretation/comments] Long after they were laid down, [fossil shells in site 2 indicate that this was in the sea], the rocks were uplifted, tilted or folded and broken by great Earth movements over millions of years. [Observations/teaching points] 
The rocks are now 100 metres above sea level. Here the beds slope [dip] gently southwards [use a compass] and are broken by cracks called joints.
DRY/KS2/TT - Earth Science On-Site