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RocksRocks
IgneousMetamorphicSedimentary
What is a Rock?
• A rock is composed of minerals
• Can be made of organic material
• Solid material that forms Earth’s hard surface.
Igneous RockIgneous Rock
Igneous Rock
• Rock that crystallizes from cooling of magma (inside Earth) or lava (on/outside surface of Earth)
• Characterized two ways – INtrusive or Extrusive
• Geology Kitchen Video - Igneous Rocks
• Crystallizes inside of Earth from magma
• Magma cools slowly (because of the blanket of the Earth’s layers)
IntrusiveIntrusive Igneous Rock Igneous Rock
Intrusive Igneous Rock (continued)
• Cooling slowly = large interlocking crystals (usually two or more colors)
• Large crystals = coarse-grained texture
Devils Tower, Wyoming
Igneous Intrusive Rock Samples
GraniteGranite
Note 3 minerals = mica (black)Note 3 minerals = mica (black)quartz (smoky)quartz (smoky)feldspar (pinkfeldspar (pink))
ExtrusiveExtrusive Igneous Rock Igneous Rock
• Crystallizes outside of Earth from lava – mostly from volcanic activity
• Lava cools quickly• Cooling quickly = tiny or no
mineral grains (usually one drab color)
Extrusive Igneous Rocks (Continued)
• Tiny or no mineral grains = fine-grained texture
• EXTRA : Sometimes has pores or holes from trapped gases
Extrusive Igneous Rock Samples
PumicePumice
Basalt (seafloor)Basalt (seafloor)
ObsidianObsidian (volcanic glass)(volcanic glass)
Notice the very smooth texture
Notice the drab colorNotice the holes or pores
MaficMafic vsvs FelsicFelsic
• Mafic igneous rocks - dark in color and have a high density due to high quantities of heavy elements (magnesium, iron, calcium and sodium)– basalt (extrusive) and gabbro (intrusive).
• Felsic igneous rocks – light in color and have a lower density due to high quantities of lighter elements (silicon, oxygen, aluminum, sodium and potassium)– Pumice (extrusive) and granite (intrusive)
Sedimentary Rock
• How does Sedimentary Rock form? • Click on image for video clip
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Sedimentary RockSedimentary Rock• Formed at surface of Earth (in lakes,
oceans, rivers) in thin or thick layers (strata)
• Layering is referred to as stratification• Formed from Cementation & Compaction
of sediments or Evaporation/Precipitation• Only rock type to contain fossils – one
exception = volcanic ash• Characterized two ways – clastic or non-
clastic
Sedimentary Rock Strata
ClasticClastic Sedimentary Rock Sedimentary Rock
• Mineral grains (sediments/fragments) are compacted and cemented together.
• Example – sand compacted and cemented = sandstone
• Example – mud/clay compacted and cemented = shale
• Example – pebbles, sand and mud compacted and cemented = conglomerate
• Geology Kitchen Video – Clastic Sedimentary Rock
ClasticClastic Sedimentary Rock Sedimentary Rock SamplesSamples
sandstonesandstone
shale fieldshale field
Non-clasticNon-clastic Sedimentary Sedimentary RockRock
• Two types – Organic Non-clastic or Chemical Non-clastic
• Organic – made from once living things – plants (coal) or animal life (fossil rich limestone - coquina)
• Chemical – made from evaporation (gypsum) or precipitation – (CaCO3 – chemical limestone)
• Geology Kitchen Video – Chemical and Biologic Sedimentary Rock
Non-clastic Sedimentary Rock Samples
Coal - organicCoal - organic
Fossil rich limestone - organicFossil rich limestone - organic
Chemical limestoneChemical limestone
Gypsum - chemicalGypsum - chemical
Sedimentary Features
• Ripple Marks – left by water or wind in sand, mud, etc. – can be preserved as a rock feature
Sedimentary Features
• Mud cracks in today’s puddles can be preserved as rock millions of years from now
Sedimentary Features
• Cross bedding – formed in old sand dunes or on off-shore sand bars
Metamorphic RockMetamorphic Rock
• How is metamorphic rock formed?
Metamorphic RockMetamorphic Rock• Formed deep inside the Earth from
intense heat and pressure • Any rock type can be changed by
metamorphism – depends on how much heat, pressure and original rock type to determine the outcome
• No melting involved – solid state process (more like softening)
• Hardest of three types of rock• Characterized two ways – foliated or
non-foliated• Geology Kitchen Video - Metamorphism
FoliatedFoliated Metamorphic Metamorphic RockRock
• Banding (stripes) or cleavage (flaky) is present
• Always a change structure and texture of original rock and sometimes a change in the composition.
• When composition changes – most often a semi to precious gem can be formed.
• Animation of metamorphism forming foliated rock
• Generally created from a rock that had more than one color.
FoliatedFoliated Metamorphic Rock Metamorphic Rock SamplesSamples
schistschist
Gneiss (Previously granite)Gneiss (Previously granite)
Slate (previously shale)Slate (previously shale)
Non-foliatedNon-foliated Metamorphic Metamorphic RockRock
• NO Banding and/or NO cleavage
• Change in structure and texture of original rock
• Possible change in composition.
• Generally created from rocks with only one color
Non-foliatedNon-foliated Metamorphic Metamorphic Rock SamplesRock Samples
Quartzite Quartzite (previously sandstone)(previously sandstone)
Marble Marble (previously limestone)(previously limestone)