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Classifying Rocks Rocks
-naturally occurring solid mixture of one or more minerals and organic matter -make up Earth’s crust
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Geologists Texture -persons that collect and study rocks
-observe texture and color -determine mineral composition -look and feel of rock’s surface -ex. smooth, glassy, rough, chalky
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Grains -particles of minerals that give rock texture Size
-large grains = coarse grained -small grains = fine grained
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Shape of grains Pattern -wide range of different shaped grains -ex. fine pieces of sand, small seeds, smooth, jagged -grains form patterns -ex. flat layers, swirling patterns
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-forms from cooling of molten rock
Not visible Igneous Rock -no visible grain happens with fast cooling -forms from cooling of molten rock
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The Rock Cycle The three main types of rock are formed during the rock cycle.
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Igneous Rock -any rock formed magma or lava cooling -“igneous” means “fire” -made of mineral crystals -exception: different types of volcanic glass -hard, dense, and durable -used for tools & building materials -classified by: origin, texture, & mineral composition
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Origin Extrusive Rock -where they are formed -two types: extrusive and intrusive -formed from lava erupting on Earth’s surface Fast cooling Small crystals -ex. Basalt and Obsidian
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Intrusive Rock -formed when magma hardens below the surface Larger crystals Slow cooling magma -ex. Granite; forms core of many mountains
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Sedimentary Rock -forms from other rock, plant, & animal remains pressed together -forms in layers
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Sedimentary Rock Sediment
-forms from particles being weathered, eroded, and deposited by water and wind are cemented together. -small, solid pieces of materials that come from rock or living things *other things include: shells, bones, leaves, stems
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Erosion Deposition -running water or wind loosen and carry away fragments of rock -sediment settles out of water or wind carrying it -after deposited; compaction and cementation change the sediment
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Compaction -process that presses sediments together -happens over millions of years -each year forms new layers compacted together -minerals in rock dissolve in water during compaction
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Cementation -dissolved minerals seep into spaces -process where dissolved minerals crystallize and glue particles of sediment together
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Types of Sedimentary Rock
Clastic Rock -3 major groups: 1. clastic rock 2. organic rock 3. chemical rock -rock fragments are squeezed together -grouped by size of rock particles of which they’re made
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Shale Sandstone -forms from tiny particles of clay -water deposits clay in very thin layers -feels smooth & splits easily -forms from sand on beaches, ocean floor, riverbeds -sand is compacted and cemented -easily absorbs water
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Conglomerate & Breccia
-mixture of fragments of different sizes -round edges are conglomerate -sharp edges are breccia
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Coal Organic Rock -made from living things
-remains of swamp plants buried in water -layers of decaying plants are squeezed -forms coal over millions of years
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Limestone -formed from coral, clams, oysters, and snails whose shells pile up -shells are made of calcite -calcite cements shells together to form limestone
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Chemical Rocks Uses of Sedimentary Rock -minerals dissolved in solution crystallize -also when seas evaporate and leave mineral deposits -ex. rock salt, gypsum -used in building materials -decorating outside walls of buildings -limestone used in cement
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-formed when existing rock is changed by heat, pressure, or chemical reactions
Meta (changed) Morphos (shape) -forms deep underground Metamorphic Rocks
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How Metamorphic Rocks Form
-collisions of Earth’s plates push rocks downward -deeper a rock is buried, the greater the pressure and temperature.
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Classifying Metamorphic Rocks
Foliated -classify by arrangement of grains -grains arranged in parallel layers or bands -thin, flat layering -may split apart along bands -ex. slate, gneiss
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-grains arranged randomly
-do NOT split into layers -ex. marble & quartzite -marble (formed from limestone) used for buildings and statues -slate (formed from shale) used for flooring, roofing, walkways, & chalkboards Nonfoliated Uses of Metamorphic Rock
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Rock Cycle -continual process by which new rock forms from old rock material -Earth’s constructive and destructive forces, like plate tectonics, move rocks through cycle
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Plate Tectonics -force that drives the rock cycle -push rocks back into the mantle where they melt and become magma -causes folding, faulting, & uplift that move the rocks -two types cause movement of rocks: 1. Subducting Oceanic Plates 2. Colliding Continental Plates
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