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Geology 12 Geology 12
Presents
Chp 4 Volcanics (& Plutonics) Intrusive igneous body = pluton = when magma intrudes into and solidifies in the crust. They are later exposed due to weathering & erosion
•2 types: Concordant & Discordant
•A: Concordant: boundaries of pluton parallel to layers in country rock.
•sills & laccoliths
A: concordant features: intrusion runs parallel to
bedding• 1. sill: usually <1 m thick (but up to 300 m
thick
• Parallel to bedding structures
• Has inclusions of country rock & contact metamorphism in top & bottom
• No vessicles (bubbles)– Ex: Palisades of New York
1. Sill: 1. Sill:
• 2. Laccolith: mushroom top sill where overlying rock is pushed up “zit”– Ex: Black Hills, S.D.
Laccolith : concordantLaccolith : concordant
Laccolith : concordantLaccolith : concordant
Laccolith : concordantLaccolith : concordant
Black Hills, SD
Black Hills, SD
Black Hills, SD
• B: Discordant: boundaries of intrusion cut across layering of country rock.– Dikes, pipes, stocks/batholiths
• 1. Dikes: 1-2 m thick (but some cm to 100s of m thick
Dike: discordantDike: discordant
Volcano
Dike: Dike: discordantdiscordant
Dike: discordantDike: discordant
Ship Rock, AZ.
Volcanic neck
• 2. Volcanic Pipe: solid lava conduit from magma chamber to surface– Mined for diamonds in northern Canada.
VolcanoNeckAfterBefore
Pipe
Magma Chamber
Volcanic Pipe: discordantVolcanic Pipe: discordant
Ekati Mine, NWT
Volcanic neck
Volcanic neck
Devils Tower, WY.
• 3. Batholith: largest intrusive body with >100 km2 of exposed surface area– Stock: <100 km2 of exposed surface area– Usually granite
Stock
Stock
Batholith
XenolithBefore After
Batholith: discordantBatholith: discordant
Batholith: Batholith: discordantdiscordant
Batholith: discordantBatholith: discordant
Batholith: discordantBatholith: discordant
Chief
Stock: discordantStock: discordant
Extrusive igneous body: structures created by magma -> lava solidifing (Volcanics) on the Earth’s surface.550 active volcanoes (60% on Ring
of Fire, 20% in Mediterrean, rest mainly on divergent boundaries)
Emit many gasses: H2O (50-80%), CO2, N2, SO2, H2S (+ some CO, H2,Cl2).
• Types of Lava: Type of Lava Volcano Type Location Viscosity Colour
Felsic/silisic composite convergent thick/hi light
dome ocean\cont
intermediate cinder cone
ocean\ocean
Mafic shield divergent thin/lo dark
basalt flood
cinder cones hot spots
Exp
losi
ve
&
Subduction: Oceanic\Cont’lSubduction: Oceanic\Cont’l
Subduction: oceanic\oceanicSubduction: oceanic\oceanic
DivergentDivergent
Hot SpotsHot Spots
• Lava Flows & Pyroclastic Material
fire + pieces blown out of volcano
A: Lava Flows:
1. Pahoehoe: ropey, cow pie lavaFrom thin mafic
Play pahoehoe movie
Lava Flows: PahoehoeLava Flows: Pahoehoe
Lava Flows: PahoehoeLava Flows: Pahoehoe
Ford Tough
• 2. Aa: rough, jagged, angular blocks of lava
– As lava freezes, it is being moved and breaks into pieces like glass.
Lava Flows: AaLava Flows: Aa
Lava Flows: AaLava Flows: Aa
3. Columnar Jointing: lava 3. Columnar Jointing: lava cools, contracts and splits at cools, contracts and splits at 60’ angles into hexagonal 60’ angles into hexagonal columnscolumnsMainly mafic lavaMainly mafic lava
Lava Flows:Columnar JointingLava Flows:Columnar Jointing
• 4. Pillow lava: blobs of lava quickly freeze underwater into “pillows”
Lava Flows: Pillow LavaLava Flows: Pillow Lava
B: Pyroclastic Material = Tephra = lava ejected into air• 1. Ash: < 2mm
– Most common pyroclastic– Welds to form tuff– Can be ejected 2 ways:
• A) Ash Fall: blown high into atmosphere & may travel 1000s of km before settling
–Can cool climate for years (ice age?)• B) Ash Flow= Nuee Ardente = Pyroclastic
Flow: horizontal blast of ash and gasses–+500C at 800 km/h–Mt St Helens, Martinique
Pyroclastics: AshPyroclastics: Ash
Pyroclastics: AshPyroclastics: Ash
Pyroclastics: Ash FallPyroclastics: Ash Fall
Pyroclastics: Ash FlowPyroclastics: Ash Flow
Animation
• 2. Lapilla: 2-64mm = pebble size
Pyroclastics: LapillaPyroclastics: Lapilla
• 3. Blocks: solid chunk of igneous rock >64mm blown out of volcano
Pyroclastics: Pyroclastics: BlocksBlocks
• 4. Bombs: blob of hot molten lava >64mm that is ejected, and partially freezes in flight.
molten
solid
Pyroclastics: BombsPyroclastics: Bombs
• Volcano: conical mountain formed around a vent
• Crater: depression near summit of volcano
• Caldera: huge depression when most of volcano falls back into magma chamber
COCO22 being being emitted with emitted with a pipe from a a pipe from a
lake in a lake in a dormant dormant
volcano in volcano in AfricaAfrica
• Types of Volcanoes
• 1. Composite/Strato: composed of layers of pyroclastics and lava flows– Andesitic rock usually (intermediate lava)– Ex. Mt. Baker, Mt. Vesuvius, Mt Fuji
LavaAsh
30’
Volcano: Composite/StratoVolcano: Composite/Strato
Mt. Rainier
Mt. St. Helens
Fuego, Mexico
Mt. Jefferson
Mt. Washinton
Mt. Shasta
Three Sisters & Black Butte
• Lahar: mudflow of ash & water
– Kill 1000s
– Tacoma is built on old lahars!
– *Lahars and Pyroclastic flows pose the greatest human danger from volcanoes
Volcano: lahar mud flowVolcano: lahar mud flow
• 2. Lava Dome: very, thick felsic/silisic lava moves up slowly under immense pressure– Ex: Lassen Peak, CA, inside of Mt. St. Helens
Old volcano
Dome
Lassen Dome, CA
Volcano: Lava DomeVolcano: Lava Dome
• 3. Cinder Cones: short-lived “baby volcanoes consisting of just pyroclastics– Form from initial eruption– Up to 400 m high
33’
Volcano: Cinder ConeVolcano: Cinder Cone
• 4. Shield: shallow sloped consisting of many low-viscosity mafic lava flows– Largest volcanoes on Earth– Ex: Hawaii (10 km high = BIG)
10’
Volcano: ShieldVolcano: Shield
• 5. Basalt Flood/Basalt Plateau: large flows of low-viscosity mafic lava that flow from long fissures (crack), rather than a single vent.– Result of divergent boundaries
Volcano: Basalt FloodVolcano: Basalt Flood
One flow
•Cumulative flows in Washington are over 1 mile thick
One flow
Melting RockMelting Rock
Mantle rock is solid, magma is only Mantle rock is solid, magma is only present under certain conditionspresent under certain conditions
Factors that affect melting includeFactors that affect melting includeTemperatureTemperaturePressurePressureVolatiles (water, gas)Volatiles (water, gas)
TemperatureTemperature
Geothermal gradient, temperature Geothermal gradient, temperature increases 25 celsius every km depthincreases 25 celsius every km depth
Melting temperature of rocks at the Melting temperature of rocks at the surface is between 750-1000celsiussurface is between 750-1000celsius
Different minerals melt at lower Different minerals melt at lower temperatures, this produces a partial temperatures, this produces a partial melt of mantle and crust rocksmelt of mantle and crust rocks
PressurePressure
Pressure increases with depth, Pressure increases with depth, causes a higher melting temperaturecauses a higher melting temperature
• Why Magma Rises• 1. Forceful Ejection: magma moves
from high pressure at depth to low pressure at the surface
• 2. Stoping: displacement of magma by country rock (i.e. xenoliths) pushes magma up (like placing ice cubes in a glass of water)
StopingStoping
• Explosiveness of a volcano is dependent on:
1. viscosity of magma: high viscosity slows the escape of gases which expand greatly near the surface
2. “stickiness” of magma = “corking effect”. The stickier, the more pressure it requires to erupt so when it does erupt…
• Higher silica increases both viscosity & stickiness
Do Lab 4-1 Igneous Rock IDDo Lab 4-1 Igneous Rock IDDo WS 4.1Do WS 4.1Do Chps 3-4 Review WSDo Chps 3-4 Review WS