Created by eimearkelly3
over 11 years ago
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Question | Answer |
Sediments are transported by | wind, water, and ice |
process of lithification | compression, compaction, cementing |
layers in sedimentary rocks | strata |
rocks are broken down into sediments by | denudation (weathering and erosion) |
Rocks are destroyed at | Subduction zones |
Igneous rocks are formed by | Magma/lava cools and becomes solid |
examples of igneous rocks | basalt, granite, pumice |
Sedimentary rocks form | Sediments (plants, remains of animals, rocks), accumulate, compress, compact, and cement into a solid |
examples of sedimentary rocks | limestone, shale, sandstone, conglomerate, coal |
Metamorphic rock is formed by | rocks being changed by great heat and/or pressure |
examples of metamorphic rocks | marble, quartzite, gneiss, slate, schist |
Types of igneous rocks | Plutonic (Intrusive) Volcanic (Extrusive) |
Plutonic (intrusive) rock | Granite |
Granite forms | when magma cools slowly within the Earth's crust |
Granite has _____ crystals because | Large crystals because the magma cooled slowly |
Granite is _______ in texture | Coarse |
Colour of granite and why it varies | The colour of granite varies from white, grey, pink, to black. It varies because of different percentages of the minerals mica, feldspar, and quartz. |
Granite formed ______ million year ago during the ________ foldings | Granite formed 400 million years ago during the Caledonian foldings |
Where can granite be found? | The Mourne Mountains Co. Down The Dublin-Wicklow Mountains - The Leinster Batholith |
Granite is ______ and ______ and is therefore used for ___________ | Granite is strong and resistant and is used as a building material |
Other uses of granite | Kitchen worktops Fireplaces |
When granite is weathered it produces | Clay |
Volcanic (extrusive) rock | Basalt |
Basalt formed when | Magma cooled outside the Earth's crust |
Size of crystals in basalt and why | Small crystals (microscopic) because the lava cooled quickly when it was exposed to the elements |
Texture of basalt | Fine-to-medium-grained |
Colour of basalt | Black to dark grey |
Minerals in basalt | Feldspar, quartz |
Properties of basalt and what they make it appropriate for | Hard, resistant Used for road construction (too dark for buildings) |
Where can basalt be found | The Antrim-Derry Plateau --> The Giant's Causeway |
Sedimentary rocks form from | The build up of sediments over millions of years |
Process of lithification | Accumulation, compression, compaction, and cementing into solid rock |
Layers in sedimentary rock | Strata |
Horizontal weaknesses in sedimentary rock | Bedding planes |
Vertical weaknesses in sedimentary rocks | Joints |
Permeability of sedimentary rocks | Permeable |
examples of organic sedimentary rocks | limestone, coal |
examples of inorganic sedimentary rocks | sandstone and conglomerate |
Organic sedimentary rocks come from | The remains of once living organisms e.g. plants and animals |
Organic sedimentary rock | Limestone |
Formation of limestone | Limestone formed on the bed of warm, tropical, shallow seas about 350 million years ago when Ireland lay close to the Equator (Carboniferous era) |
Process of lithification in limestone | Over time the bodies of dead marine creatures e.g. shells, coral, teeth, skeletons etc. accumulate on the sea floor. The weight of water and the great weight of the water caused compression, compaction, and cementing into solid limestone. |
Cement in limestone | Calcium carbonate from shells |
Limestone is weathered by | Carbonation |
Limestone may contain | Fossils as it forms at temperatures that do not destroy fossil remains. |
Colour variation in limestone and why | Limestone varies in colour white to grey to black depending on impurities in the water. |
Uses of limestone | Cement and in construction |
Where is limestone found and what kind of landscape is it? | The Burren Co. Clare - Karst landscape |
Chalk | Pure white form of limestone |
Inorganic sedimentary rocks form from | The remains of pre-existing rocks e.g. sand, clay, pebbles |
Sediments are transported by ______ to _____ | Sediments are transported by wind, water, and moving ice to lakes, oceans and seas. |
Lithification of inorganic sedimentary rocks | Sediments are compressed, compacted, and cemented under the weight of water and overlying layers |
Inorganic sedimentary rock | Sandstone |
Where can sandstone be found in Ireland? | The mountains of Munster e.g. Caha |
sandstone in Munster is also known as | old red sandstone |
texture of sandstone | coarse |
colour of sandstone and why | red or brown because of the presence of iron oxide |
Formation of sandstone | Sandstone formed 400 million years ago, when Ireland had a desert type climate. It formed when sand or quartz deposited on land or in water were compressed and cemented together. |
Sanstone is porous which means | that it can hold oil or gas |
Uses of sandstone | building rock e.g. front of houses and road chippings |
Where can sandstone be found? | Comeragh mountains Co. Waterford Magillycuddy's Reeks Co.Kerry |
Shale | Clay compacted |
Coal | Vegetation |
mudstone | mud |
Metamorphic rocks are formed | when igneous or sedimentary rocks under change due to great heat and/or pressure |
Thermal/contact metamorphism | When heat causes the rocks to change/metamorphose |
Types of metamorphism | Regional/dynamic Thermal/contact |
examples of metamorphic rocks | marble, quartzite |
Effects of metamorphism on: hardness colour chemical composition foliation | Rock is harder than original Colour may change due to the effect of heat Mineral crystals may be rearranged to form foliated metamorphic rock e.g. gneiss Heat and pressure may cause the rock minerals to recombine to form different minerals in the metamorphic rock. |
Sandstone that changed due to great heat and pressure | Quartzite |
The spaces between the grains of quartz are filled with _____ from ______ | The spaces between the grains of quartz are filled with silica from magma |
Permeability of sandstone | The silica and quartz re packed very tightly together making quartzite very resistant to erosion. |
Colour of quarzite | light-coloured rock, often white |
Where can quartzite be found? | The peaks of mountains such as Croagh Patrick Co.Mayo and the Sugarloaf Co.Wicklow |
Uses of quartzite and why | It is a hard rock and is therefore used for road surfacing |
When limestone is changed by heat and/or pressure the resulting rock is | Marble |
Properties of marble | Hard, crystalline rock |
Colours of marble and where they can be found | Green (Connemara), white (Rathlin Island Co. Antrim), red (Cork), |
White marble comes from | Pure limestone changing in composition |
What causes marble not to be pure white and give examples | Impurities e.g. clay, silt, sand, iron oxides |
Uses of marble | Marble can be cut and polished and used for kitchen worktops, gravestones, ornaments, fireplaces, and building materials (extracting for building materials by quarrying) |
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Basalt |
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Sandstone |
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Quartzite |
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Granite |
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Limestone |
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Marble |
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