Folding + faulting Flashcards
Ductility
When rocks are heated and compressed, they can bend without breaking. Ductility + plate movement pressure = floding
Top curve of a fold
Anticline
Downward curve of a fold
Syncline
What joins syncline and anticline
limb
Symmetrical fold
same pressure on each side -Even fold
Asymmetrical fold
Pressure is slightly greater on one side -One side steeper
Overturned fold
Pressure is much greater on one side - One limb is on top of another
Recumbent fold
Pressure is so much greater on 1 side - Limbs are horizontal, moving in the same direction
Overthrust fold
Pressure is so much greater on one side that it fractures the other - one limb pushed over another
Fold mountain locations - Continental - Continental
Oceanic subducts -> pressure ->edges fold -> fold mountain on the boundary line eg.The Andes
Fold Mountain locations - Continental - Continental
Neither subducts, both move up -> heat -> ductility-> really flexible rock -> steep slopes eg Himalayas
Caledonian period - How old? What plates? Effect on Ireland?
400 mill years old
Eurasian + North American
Sugarloaf Co. Wicklow
Armorican - How old? What plates? Effect on Ireland?
250 mill years old
Eurasaian and African
MacGillycuddy’s Reeks Co. Kerry
Alpine - How old? What plates? Effect on Ireland?
60 mill years ago to now
Eurasian + Indo-Australian
Hasn’t affected Ireland
Faulting processes - Tension
Rock is pulled apart from both sides - stretches, breaks, sinks.
Normal fault
Faulting processes - Compression
Pressed together from both sides, shortens, fractures, pushes up
Reverse fault
Faulting processes - Sheering
Rock layers move sideways in opposite directions - crust ttears
Transform fault
Parts of a fault - Scarp
Cliff from vertical rock displacement
Parts of a fault - Throw
Distance the cliff moved up or down
Parts of a fault - Heave
Horizontal rock movement
Parts of a fault - Fault plane
Surface fault, rock moves on
Parts of fault - Hanging wall
Section of sliding rock
Parts of a fault - Footwall
Section of not moving rock
Normal fault example
East African Right valley - crust between 2 faults sank below sea level