Science and Engineering at The University of Edinburgh |
||||
|
||||
![[University Logo]](/icons/unilogo_25476c.gif "Link to The University of Edinburgh Home Page"){kind=icon}
Section Contents
- Introduction
- Geological History
- The Hawse
- Palaeomagnetism
- Sediment rafts
- Vesicles
- Hutton's Section
- Spheroidal weathering
- White sandstone
- Hutton's Rock
- Distorted strata
- Contact details
- Crag and Tail
- The Cats Nick
- Dykes
- Slickensides
- Dessication cracks
- Ripple marks
- Bedding
- The Long Row
- Vent Agglomerate
- Sampsons Ribs
- Geological Map
- Questions
- References
Extras
Tutors only
Distorted strata
Locality 8: The Salisbury Crags sill occasionally cross-cuts the sedimentary layers and in some places the thinly layered sedimentary rocks have been distorted during intrusion. Such features clearly indicate that the rock which forms Salisbury Crags is a sill and not a lava flow.