The Rock Cycle

Rocks are continuously being formed, changed/modified, destroyed, and reconstructed by forces within the Earth. This is known as the rock cycle.

    ROCKS ARE GROUPED ACCORDING TO THEIR FORMATION Igneous            Magma/lava cools          e.g. basalt, granite                           and becomes solid               pumice     Sedimentary     When sediments           e.g. limestone, coal                        (plants, remains of               sandstone, shale                        animals, rocks),                   conglomerate                        accumulate, compress,                        compact, and cement                        into a solid.                         Metamorphic    When a rock is               e.g. marble, quartzite (Latin for           subjected to great heat          slate, gneiss, schist change)            and/or pressure, it is                        changed.    

PLUTONIC (INTRUSIVE) ROCKS Form when magma cools slowly within the Earth's crust. It may cool at a depth of several kilometres e.g. granite. Granite has large crystals because the magma cooled slowly. Granite may be found in the Mourne mountains Co.Down which were exposed due to denudation. Granite is a strong, resistant rock and is commonly used as a building material. It is often polished and used for kitchen worktops and fireplaces. 

    VOLCANIC (EXTRUSIVE) IGNEOUS ROCKS Form when magma cools outside on the Earth's crust. These have smaller crystals because lava cools quickly when exposed to the elements e.g. basalt Basalt is composed of quartz so It is a hard, resistant rock and is therefore used for road construction. It is too dark to use for buildings. In the Antrim-Derry Plateau, lava poured out of the fissures in the ground. It cooled and contracted to form six-sided columns of basalt. e.g. The Giant's Causeway.    

Limestone --> marble e.g. Connemara Co.Galway Sandstone --> quartzite eg: Croagh Patrick Co. Mayo  

QuartziteQuartzite is sandstone which changed due to great heat and pressure. The spaces between the grains of quartz are filled with silica (from magma). The quartz and silica are packed tightly together. As a result, quartzite is very resistant to erosion.Quartzite is a light-coloured rock, which is often white in colour, and is found on the peaks of mountains such as Croagh Patrick, Co. Mayo and the Sugarloaf Co. Wicklow. Because it is hard, it is commonly used for road surfacing.