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Solid material Deposited on Earth’s surface Wind, water, ice, gravity, chemical
precipitation Form sedimentary rocks
Sediment
Earth’s crust is worn down Physical or chemical processes Clastic sediments- rock or mineral
fragments◦ Greek klastos = broken
Weathering
Removal and movement of rock fragments 4 Main ways:
◦ Wind◦ Moving water◦ Gravity◦ Glaciers
Deposition- sediments laid down◦ Land and water
http://www.youtube.com/watch?v=51C7vEAVbxk
Erosion
Sediments become rock Greek lithos = rock Layers of sediment = pressure Deep layers = hot temperature Cementation- mineral growth cements
sediment together
Lithification
Bedding- horizontal layering Graded Bedding- larger/heavier fragments
at bottom layers Cross-Bedding- layer crossing over another
one
Features of Sedimentary Rock
Preserved evidence of once-living organisms◦ Remains or impressions
Found in sedimentary rocks
Fossils
Clastic- deposited loose fragments Chemical- dissolved minerals left behind
Types of Sedimentary Rocks
Classified by sediment size Coarse-grained: gravel-sized fragments Medium-grained: sand-sized fragments Fine-grained: silt-sized fragments
Porosity- % of open spaces
Clastic Sedimentary Rocks
Evaporation- leaves minerals behind◦ Evaporites: rocks formed this way
Organic- remains of once-living organisms◦ Shells, bones◦ Coal- remains of plant material; carbon; fuel
Chemical Sedimentary Rocks
Energy- coal, natural gas, oil, nuclear Fertilizers Iron Walls/buildings Snapshot- cross bedding & fossils
Importance of Sedimentary Rocks
http://geology.com/rocks/sedimentary-rocks.shtml
Pictures of Sedimentary Rock
Temperature/pressure changes rocks◦ Composition, minerals, texture
Meta = change Morph = form
Metamorphic Rocks
Regional: large regions Contact: molten rock touches solid rock Hydrothermal: hot water alters rock
Types of Metamorphism
Foliated: minerals are wavy layers/bands Non-foliated: no mineral grains in one
directions
Metamorphic Textures
http://geology.com/rocks/metamorphic-rocks.shtml
Pictures of Metamorphic Rock