GEO 1303 Lecture Exam 2

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57 Terms

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Weathering

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Erosion

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Physical weathering

Reduces solid rock to small fragments without altering the chemical composition of rocks and minerals (Ex- gravel, sand, salt, clay sized particles)

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Chemical weathering

substances derived from solution by inorganic or biochemical processes (Ex- clay minerals and ions, compounds and solution)

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Regolith formation on Moon

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Regolith formation on Mars

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Regolith formation on Earth

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Soil degradation

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Earthquakes Causes

  • Movement along faults

  • Volcanic eruptions

  • Landsides

  • Explosions

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Seismic waves

They cause the most of the damage and shaking people feel
during an earthquake

  • Body waves travel through Earth. P wave fastest a first wave, S-wave shears material and second wave

  • Surface waves trave; along or just below the surface

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Measuring earthquakes

  • Intensity ( qualitative)- measures the kind of damage

  • Magnitude (quantitative)- measures the amount of engergy that is released

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Destruction from earthquakes

  • Ground shaking

  • Liquefaction (water-saturated clays becomes fluid during ground shaking)- ground is no longer stable and buildings fall

  • Fire-natural gas and water lines break

  • Tsunami- seafloor earthquakes generate deadly waves

  • Ground failure-landslides and rockslides

  • Human death

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Earth’s interior

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Volcanism in the solar system

  • Jupiter moon Io is the most volcanically active body in the solar system

  • Mars Volcano Olympus Mons is the tallest in the solar system

  • Venus has volcanoes and flood basalt

  • Mercury has widespread flood basalts

  • the dark parts of the moon are flood basalts

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Features of Volcanoes

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Parts of Volcanoes

  • Vent- where magma and other volcanic products erupt onto the surface

  • Crater- hole at the hop of the volcano

  • Caldera- circular depression formed from the collapse of rock above an empty magma chamber (example-Crater Lake)

  • Fissures- linear cracks along the side of the volcano that magma can also erupt from

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Volcanic gases

  • Mostly water vapor

  • Also contains CO2, SO2, HS, N2

  • Very small amounts of C), Hydrogen, and chlorine

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Flood basalts

involve HUGE volumes of magma and represent the largest basalt eruptions on Earth. (example-Columbia Plateau)

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Volcanic hazards

Basaltic

  • Lava Flow

  • Volcanic ash

  • Lava/fire fountain

  • Lahar

  • Pyroclastic flow

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Locations of volcanoes

Most are found at plate boundaries (60% are at the ring of fire)

  • Divergent plates are mostly mafic sheild volcanoes with pillow basalts

  • Convergent plates and subduction caused the ring of fire. They form intermediate or felsic volcanoes

  • Intraplate (hot spots) form mafic shields (Hawaii)

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Depositional environments

A geographic setting where sediment
is accumulating. Determines the nature of the sediment that accumulates

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Depositional environments resulting rock types

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Detrital sediments Formation

  • Conglomerate-forms in water

  • Breccia- forms with little water

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Detrital sediments classification

  • Conglomerate- well rounded pebble sized clast. Mix of sand slit or clay

  • Breccia- angular pebble sized clasts with sand silt or clay

  • Sandstone-sand sized grains, layers

  • Shale- very fine grained clay particles that breaks in chips

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Detrital sediments types

Gravel, Boulder, Cobble, Pebble, sand, mud, slilt, and clay

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Chemical sedimentary rocks classification

  • Evaporites- rock salt and rock gypsum, Chemcial sediments formed by precipitation of a mineral during the evaporation of water. Forms in dired up lakebed

  • Carbonate- limstone and dolostone, primarily containing the carbonate ion such, forms when magnesiu replaces some calcium in limstone. Forms in calm saltwater

  • Coal- composed of altered land plant remains

  • Chert- flint and jasper, forms in deep marine, microcrystalline quartz

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Sedimentary facies

Sediment or sedimentary rocks that are recognizably
different from adjacent sediment or sedimentary rocks
and are deposited in a different depositional
environment. Sea levels either increase or decrease to create these

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Bedding types

  • Cross bedding- perserves layers deposited at an angle. Sand dunes and shallow marines.

  • Graded bedding- largest heavist particles settel first and then smaller particles on top

  • Parallel bedding-This type of bedding typically forms in environments with relatively low energy, allowing sediments to settle uniformly and create distinct layers that run parallel to each other.

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Sedimentary structures

  • Currnet ripple marks- asymmetric ripple marks

  • Wave formed ripple marks- symmetrical shappe ripple marks

  • Mud cracks-when mud dries out and leaves cracks

  • Fossils- remains and traces of ancient life

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Petroleum Gas

Made from microoganism,Oil gets trapped in sandstone

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Sedimentary rock resources

Sand and gravel
 Clay
 Coal
 Limestone
 Phosphates
 Gold, uranium, and other
metals
 Salt
 Gypsum (used in drywall)
 Banded iron formations
 Petroleum (oil and
natural gas)

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Metamorphism

transformation (change) of rocks without melting, usually beneath Earth's surface. Caused by heat, pressure, or fluids

Contact-high temp low pressure

Dynamic- when rocks are crushed. high pressure low temp

Regional-msot common, found at convergent plates. High temp and pressure.

Meteorite impact- ultrahigh temp, ultrahigh pressure

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Metamorphic grade

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Index minerals


the degree of metamorphic change a rock

has undergone, usually listed as low(small change), intermediate (medium change), or high (large amount of change)

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Classification of metamorphic rocks

Foliated textures are produced
by the preferred orientation of
platy minerals, such as
muscovite, because of pressure

Nonfoliated textures do not
have preferred orientation of
minerals (minerals are
randomly oriented)

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Metamorphic facies


a group of rocks containing a distinctive mineral assemblage formed under similar conditions of temperature and pressure

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Metamorphic mineral and rock resources

Slate Marble Gneiss. Graphite, Talc, Garnet, Metallic ores

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Shield Volcano

  • Looks like Captain America’s shield sitting on the ground

  • Gentle slopes

  • Basalt

  • Non explosive and poses little danger to humans

  • Begins with a lava/fire foundation. Scoria forms a cinder/scoria cones in a few months

  • low viscosity (more fluid)

<ul><li><p>Looks like Captain America’s shield sitting on the ground</p></li><li><p>Gentle slopes</p></li><li><p>Basalt</p></li><li><p>Non explosive and poses little danger to humans</p></li><li><p>Begins with a lava/fire foundation. Scoria forms a cinder/scoria cones in a few months</p></li><li><p>low viscosity (more fluid)</p></li></ul><p></p>
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Cinder/ Scoria Conde Volcano

  • Steep-sloped rarely exceeding 300m high

  • Mafic compositions

  • Found with shield volcanoes

  • Scoria and other pyroclastic materials

<ul><li><p>Steep-sloped rarely exceeding 300m high</p></li><li><p>Mafic compositions</p></li><li><p>Found with shield volcanoes</p></li><li><p>Scoria and other pyroclastic materials</p></li></ul><p></p>
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Composite Volcano

  • Composed of layers of lava flow, pyroclasitc debris and volcanic mud flows

  • Explosive and most dangerous to humans

  • Volcanoes rimming the pacific ocean are mostly these types

  • most have intermediate compositions

  • Tephra is pyroclasitc material that ejected during eruption

  • Eruption columm is tephra and gas that rises upwards into the atmoshphere

  • Pyroclastic flow forms when eruption column collapses as a dense, swirling cloud of hot gases, volcanic rock and ash

  • Lahar is rain and snowmelt mixing with lose ash and rock

<ul><li><p>Composed of layers of lava flow, pyroclasitc debris and volcanic mud flows</p></li><li><p>Explosive and most dangerous to humans</p></li><li><p>Volcanoes rimming the pacific ocean are mostly these types</p></li><li><p>most have intermediate compositions</p></li><li><p>Tephra is pyroclasitc material that ejected during eruption</p></li><li><p>Eruption columm is tephra and gas that rises upwards into the atmoshphere</p></li><li><p>Pyroclastic flow forms when eruption column collapses as a dense, swirling cloud of hot gases, volcanic rock and ash</p></li><li><p>Lahar is rain and snowmelt mixing with lose ash and rock</p></li></ul><p></p>
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Lava Domes

  • Viscous and usually felsic or intermediate lavas are forced up through the conduits of some volcanoes

  • these erupt explosively

<ul><li><p>Viscous and usually felsic or intermediate lavas are forced up through the conduits of some volcanoes</p></li><li><p>these erupt explosively</p></li></ul><p></p>
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Elastic Rebound theory

  • Rocks deform

  • Rocks rupture when pressure builds in rocks on either side of a fault to a level l which exceeds the rocks strength

  • Rocks rebound and returns to original shape when pressure is released

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<p>Name that Feature</p>

Name that Feature

S-wave, can only travel through solids

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<p>Name that feature</p>

Name that feature

1- Focus/hypocenter

2- Epicenter

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<p>Name that Feature</p>

Name that Feature

S-wave shadow zone- blocks where s waves can go because it is liquid

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<p>Name that feature</p>

Name that feature

The ground becoming no longer stable because of liquefaction

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<p>Name that feature</p>

Name that feature

P-wave, travels through solids and liquids, fastest wave

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<p>Name that feature</p>

Name that feature

Effects of a tsunami

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<p>Name that feature</p>

Name that feature

P-wave shadow zone- the core diffracted the p-wave some little make it to the surface in this area

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What happened in Pompeii in the year 79?

Vesuvius covered the city in pyroclastic flow

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Which is NOT a type of physical weathering

Hydrolysis

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Which is the term for the spot on the surface directly above where the earthquake occurs?

Epicenter

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Which of the following is involved in regolith formation on mars?

  • Meteorite impact

  • water

  • wind

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Which of the below volcano types would you expect to form fro the highest viscosity magma?

Composite

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Which of the following is the most common and destructive earthquake hazard?

Ground shaking

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Which mineral on Bowne’s reaction series is most resistant to weathering?

Quartz

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Volcanoes found at subduction zones are mostly _____; volcanoes found at hot spots are _____.

Composite, shield