Formation of Metamorphic rock
Regional metamorphism
Large areas of rock
Plate movement cause pressure on rocks
Moved down into crust
Heated and metamorphosied
Combination of heat and pressure
Gneiss from granite
Mayo
Schist from slate
Kerry
Thermal metamorphism
Rock heated extremely
Molten magma in contact with rock
Edges of dykes, batholiths and sills
Recrytallsation of rock crystals
Quartzite from sandstone
Found in Donegal
Marble from limestone
Found in connemara
Dynamic metamorphism
Plate movement
Pressure causes harder rock types
Sticky powder caused at fault lines (fault gouge)
Slate formed from shale
Formation of limestone
Inorganic
Lithification of rock fragments
Sandstone
Particles of other rocks accumlate
During lithification silca glues grains together
Permable rock
Formed when ireland was near equator
Old red sandstone found in cork and kerry
Used to be long river across ireland carrying sediments which formed these mountains
Organic
Limestone
Formed from build up of sea sediments
Formed when Ireland lay near equator
Formed in shallow seas
Grains cemented by calclium carboate from shells
Clare, the Burren
Coal
Decaying vegetation accumulated on waterlogged soil causes peat
Futher compaction takes water out creating coal
Chemically
Found in evaporated lakes in hot climates
Gypsum
37% water dissolved
Rock salt
93% of water dissolved
Both rock types found in Carrickfergus, County Antrim
Formation of igneous mountains
Intrusive rock
Plutonic rocks form when magma cools slowly
Inside earths crust
Large crystals of
Quartz
Feldspar
Mica
Granite
Grey in colour
Batholiths are example of intrusive rock
Wicklow mountains
Intermediate/hypabyssal
When magma makes way closer to earths surface and cools quicker than plutonic rock
Smaller crystals
Dolerite
Fair head sill, county Antrim
Volcanic/extrusive
Basalt
Magma reaches the earths surface
Cools as lava
Microscopic crystals
Dull grey/brown colour
Giants causeway