Folding and Faulting Flashcards
Tectonic forces that change the rock structure on the earth
TENSION, COMPRESSION, SHEARING
Tension
Plates separate and lengthen or stretch and break apart
Compression
Plates collide, rocks are squeezed and shortened causing them to fold or fracture
Shearing
Plates slide past eachother
Process of folded structures
Continental plate is compressed by forces acting on both sides, flat body of rock buckles, doesn’t fracture due to flexibility of plates and time scale (long time)
Anticline
Layers of rock that fold upwards
Syncline
Layers of rock that fold downwards
Limb
Sides of the fold that join anticline and syncline
Symmetrical fold
Limbs on each side are the same in length and steepness
Asymmetrical fold
Limbs on either side are different in length/steepness
Overfold
One limb pushes over the top of the other
Recumbent fold
When both limbs are moving in same direction causing large overhang
Orogeny
Mountain building period caused by folding and faulting e.g Caledonian
Trend
General direction in which something is developing
Denudation
The breakdown of rock by weathering or erosion
Caledonian folding
- 400M years ago
- Ocean floor subducted and sea floor buckled up
- Magma intruded into gaps in unfolds to form igneous rocks and metamorphic rocks
- Large crystals formed
- ORIGINALLY higher than any other
Armorican Folding
- 250 million yrs ago
- East to west directional trend
- Never reached the height of Caledonian folding
- Caha Mountains or Comeraghs
Alpine folding
- Reached peak 30M years ago
- Subduction didn’t occur
- Current highest mountains
Faulted Structures
Compression, tension leads to fractures and weakness, strata displaced at fault line
Case study: East African Rift Valley
- 20M yrs ago
- 4,800km from Syria to Zambezi river
- Magma plume caused continent to bulge
- Rift valley formed
- Subsided land is 153m below sea level
- Widens at 4mm per year
- Eventual split of plate
- Mt. Kilimanjaro formed due to Magma rising through weakness in rock
Faults resulting from compression
- Reverse Fault
Forms at convergent plate boundaries when compression in the earth’s crust causes fractures.
Compression: Thrust Fault
Found in areas where one plate is being subducted under another, fault at 45° or less
Compression: Block Mountain or Horst
Compression creates two parallel faults and a large block of land between faults gets pushed upwards.
Shearing: Tear Fault
Occurs at transform boundaries where rocks at edge of plate can lock. Earthquakes can occur