Rock Types
Within the three major categories of igneous, sedimentary and metamorphic, geologists recognise many more specific rock types.These are classified according to their appearance and composition, and according to the conditions in which they formed.
Dalkey Quarry
Former quarry at Dalkey Hill, Co. Dublin - the source of the granite rocks used to build Dun Laoghaire harbour.
Photo courtesy of Arnold Horner 2006.Dalkey Quarry
Former quarry at Dalkey Hill, Co. Dublin - the source of the granite rocks used to build Dun Laoghaire harbour.
Photo courtesy of Arnold Horner 2006.
Igneous rocks are divided between those which reached the surface and so were extrusive, and those which cooled near but below the earth's surface and so can be considered intrusive.
Basalt
Basalt's black volcanic rock texture and small crystals can be seen in this photograph.
Copyright Geological Survey of Ireland 2006.
Dun Laoghaire Harbour
This is built with granite rock quarried from Dalkey Hill, Co. Dublin.
Photo courtesy of Arnold Horner 2006.
Slate Quarry at Valentia Island, Co. Kerry.
These metamorphic rocks make good roofing and paving materials.
Photo courtesy of Arnold Horner 2006.Slate Quarry at Valentia Island, Co. Kerry.
These metamorphic rocks make good roofing and paving materials.
Photo courtesy of Arnold Horner 2006.Ripple Marks
Ripple marks are sometimes evident on sedimentary rocks formed in shallow water.
Courtesy of Arnold Horner 2006.
Metamorphic rocks can likewise be subdivided, some of the major types being quartzites, slates, schists, and gneisses. The Valentia Island slate quarry flouished during the nineteenth century. Valentia slate was exported to Britain and used to roof the House of Commons in London.
Gallery
Limestone
An illustration of the sedimentary rock limestone.
Copyright Geological Survey of Ireland 2006.Limestone - Copyright Geological Survey of Ireland 2006.
Quartzite Rock
This metamorphic rock consists of recrystallised sandstone combined with quartz.
Copyright Geological Survey of Ireland 2006.Quartzite Rock - Copyright Geological Survey of Ireland 2006.
Slate
This metamorphic rock is commonly found in areas with high tectonic areas. With further metamorphism, slate turns to phyllite, then schist or gneiss.
Copyright Geological Survey of Ireland 2006.Slate - Copyright Geological Survey of Ireland 2006.
Schist Rock
The somewhat course-grains can be seen clearly here.
Copyright Geological Survey of Ireland 2006.Schist Rock - Copyright Geological Survey of Ireland 2006.
Gneiss
The granular texture can clearly be seen here.
Copyright Geological Survey of Ireland 2006.Gneiss - Copyright Geological Survey of Ireland 2006.
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