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Earth's mechanical layers in order
lithosphere, asthenosphere, mesosphere, outer core, inner core
earth's compositional layers in order
crust, mantle, core
oceanic crust
thinner, more dense, younger crust making ocean floor; about 6-7 km thick
continental crust
portion of crust that primarily contains granite, is less dense than oceanic crust, and is 20-50 km thick
plate tectonics
theory that describes the lithosphere as a dozen large plates that move from convection in the solid mantle
what causes convection in the mantle?
heat flowing from the core and rising
What is concentrated along plate boundaries?
earthquakes, volcanoes, & topography
Topography
land formations on earth's surface that break smooth curvature (largest being continents & oceans); measured above sea level
divergent boundaries
plate boundary where new lithosphere is created from mantle becoming liquid & rising so plates move away from each other
convergent boundaries
plate boundary where lithosphere is destroyed & plates move towards each other
transform boundaries
a boundary where two plates slide past one another without creating or destroying lithosphere; special case of a strike-slip fault occurring at a plate boundary
mid-ocean ridge
occur along divergent plate boundaries; an underwater moutain chain where new ocean floor is formed
mid-ocean ridge process
hot mantle rock rises --> melt forms under lithosphere --> new lithosphere forms once magma erupts/rises to the surface as seafloor spreads
magnetic anomalies
pattern of long, narrow bands of high or low magnetic intensity (based on variation of magnetism of rocks) on seafloor parallel to the crest of a mid-ocean ridge
subduction zone
the region where an oceanic plate sinks down into the asthenosphere at a convergent boundary, usually between continental and oceanic plates
collision zones
a specific type of tectonic boundary where two or more tectonic plates are actively colliding with each other, often pushing rocks up & forming large mountain ranges
trench
long, narrow depressions on the seafloor that form at the boundary of tectonic plates where one plate is pushed, or subducts, beneath another (subduction zone)
typically formed at convergent plate boundaries
arc volcanoes process
occur at subduction zones where sinking oceanic plate melts & magma heats up & rises to surface from buoyant forces, leading to creation of volcanoes that form arc-shaped pattern along boundary
How do igneous rocks form?
cooling and crystallizing of magma or lava as it rises from buoyant forces (either intrusion or eruption)
How do metamorphic rocks form?
minerals re-equilibrate to combination of pressure, heat, & fluid conditions
extrusive igneous rock
igneous rock that forms when magma erupts & cools above the surface of Earth
intrusive igneous rock
igneous rock formed from the cooling and solidification of magma beneath Earth's surface
difference between rocks and minerals
Minerals are PURE - one substance. Crystalline structure.
Rocks are MIXTURES of minerals and other substances.
crystallization
process where atoms of a gas or liquid come together in proper arrangement or proportions to form a solid substance (crystal)
coarse-grained vs fine-grained texture
COARSE: grains are large enough to be seen w/ naked eye
FINE: grains not large enough to be seen
mineral
a naturally occurring, inorganic solid that has a crystal structure and a definite chemical composition
rock
naturally occurring solid mixture of one or more minerals or organic matter
igneous rock
rock that forms when magma cools and solidifies
sedimentary rock
a rock that forms from compressed or cemented layers of sediment
sediment
small, solid pieces of material found at Earth's surface as layers of loose particles from weathering & erosion, such as sand, silt, & organism shells
weathering
The chemical and physical processes that break down rock at Earth's surface.
erosion
The process by which wind, water, ice, or gravity transports soil and sediment from one location to another
metamorphic rock
A type of rock that forms from an existing rock that is changed by heat, pressure, or chemical reactions (solid-state transformation)
Where do sedimentary rocks form?
where sediment is deposited, such as ocean basins & continental margins
Where do igneous rocks form?
Mid Ocean ridges, volcanic arcs at subduction zones, hotspots
Where do metamorphic rocks form?
Deep beneath the Earth's surface in convergent margins, divergent margins, or collision zones
hotspots
places where molten material from the mantle reach the lithosphere
what two features classify igneous rocks?
texture and chemical/mineral composition
Felsic rocks
poor in iron and magnesium & rich in felsic minerals (silica & feldspar) as well as Na and K; have less pressure & more water content; tend to be lighter in color; lowest melting point (650-800 °C)
Mafic rocks
poor in silica, rich in magnesium, iron, & calcium; have more pressure & less water content; darker color; highest melting temp (1000 to 1200 °C)
what are the three types of melting?
decompression, volatile flux, & thermal (heat transfer) melting
magma chambers
large pools of molten rock that form in lithosphere as rising magmas melt & push aside surrounding solid rock
three locations of magmatism
mid ocean ridges, subduction zones (fluid-flux melting), & hotspots (thermal melting)
what is meant by extrusive/intrusive equivalent?
Extrusive & intrusive igneous rocks form 2 parallel sets of igneous rocks → identical in composition & only differed in texture
Intermediate igneous rocks
midway between felsic and mafic rocks; neither rich nor poor in silica; midway in Na, K, Fe, Mg, Ca content; melting point (800 - 1000 °C)
decompression melting
melting that occurs from a decrease in pressure w/o any additional heat
volatile flux melting
melting caused by adding volatiles (such as water); not changing pressure or temp but adding water causes rock to melt at different conditions
thermal melting
melting caused by increase of temp; occurs at hotspots
partial melt
the process by which a fraction of a rock has melted at a given temp since different minerals in rock melt at different temps (cold to hot); felsic rocks melt first
Compositions of melt & solid residue left behind differ from both each other and the starting rock
magmatic differentiation
rocks of varying composition can arise from uniform parent magma, as different minerals crystallize at different temperatures
fractional crystallization
process where liquid melt in rocks are separated from crystals formed in cooling magma (hot to cold)
creates range of mafic to felsic rocks
concordant intrusion
an igneous intrusion whose boundaries lie parallel to layers of bedded country rock
mantle plumes
a localized column of hot magma rising by convection in the mantle that causes volcanic activity in hot spots
Earth's interior temperature ______ with depth
increases
Earth's interior pressure ______ with depth
increases
Intrusive igneous rocks
rock formed from the slower cooling and solidification of magma beneath Earth's surface when rocks force their way into surrounding rock; large, interlocking composition
Extrusive igneous rocks
rock that forms from the rapid cooling and solidification of lava at Earth's surface; fine-grained texture or glassy appearance
What does the temp a rock melts at DEPEND on?
other than temp, depends on mineral composition, pressure, & absence/presence of volatiles
magma composition - hottest to coldest
HOTTEST: Ultramafic magma (low silica)
Mafic magma (basaltic)
Intermediate magma (andesitic)
COLDEST: Felsic magma (rhyolitic; high silica)
plagioclase feldspar
continuous minerals in igneous rocks where calcium (mafic) & sodium (felsic) substitute for one another in same crystal structure
Siliciclastic sedimentary rocks
Formed from clasts of primarily silicate sediments
Classified by SIZE & MATERIAL
physical weathering
takes place when solid rock is fragmented by mechanical processes, such as freezing & thawing, that do not change its chemical composition
chemical weathering
processes by which minerals in a rock are chemically altered or dissolved
types of currents
Strong currents = faster than 50 cm/s, carry gravel along w/ abundant supply of smaller particles
Moderate currents = between 20-50 cm/s, lay down sand beds
Weak currents = slower than 20 cm/s, carry muds composed of finest clastic particles
What is the driving force of chemical & biological sedimentation?
precipitation
Currents that move across Earth’s surface generally flow _______ & accumulate in ______
downhill
depressions in Earth’s crust
subsidence
broad area of crust sinks (subsides) relative to surrounding crust and forms depressions, mainly driven by plate tectonics
continental shelf
the edge of a continent that lies under the ocean
Carbonate
Sedimentary environments where sediments are rich in carbonate minerals
Evaporite
Sedimentary environments where sediments result from the evaporation of water
Siliceous
Sedimentary environments characterized by sediments rich in silica.
Wetland
Sedimentary environments associated with wetlands, often involving organic-rich sediments
Show how minerals are classified by grain type (3 groups)
Coarse-grained: gravel and conglomerate
Medium-grained: sand and sandstone
Fine-grained: silt and siltstone; mud, mudstone, and shale; clay and claystone
gravel and conglomerate
Gravel = coarsest siliciclastic sediment, consisting of particles larger than 2 mm in diameter & including pebbles, cobbles, & boulders
Conglomerate = lithified equivalent of gravel
sand and sandstone
Sand = medium-sized particles (0.62 - 2mm in diameter) that can be seen by naked eye & moved by moderate currents
Sandstone = lithified equivalent to sand
silt and siltstone
Silt = siliciclastic sediment w/ grains between 0.0039 - 0.062 mm in diameter
Siltstone = lithified equivalent to silt
mud, mudstone, and shale
Mud = siliciclastic sediment containing water where most particles are less than 0.062 mm in diameter deposited by rivers & tides
Mudstone = one equivalent of mud that are blocky & show poor or no bedding
Shale = one lithified equivalent of mud composed of silt and significant component of clay, causing them to break readily along bedding planes
clay and claystones
Clay = most abundant component of fine-grained sediments & sedimentary rocks, with particles that are less than 0.0039 mm in diameter
Claystones = rocks made up exclusively of clay-sized particles
What are carbonate sediments? Give an example of a rock it would form.
sediment formed from accumulation of carbonate materials directly or indirectly precipitated by marine organisms
EX: Limestone = dominant biological sedimentary rock lithified from carbonate sediments & composed mainly of calcite
What are evaporite sediments? Break them down further into their 2 subcategories.
chemical sediment that is precipitated from evaporating seawater or lake water
Marine evaporites = formed by seawater
Non Marine evaporites = form in arid-region lakes
Energy (force of materials moving) of environment is critical for what?
control on particle size
Transport mechanisms = ice, air, water
High energy environment
can carry large grains like cobbles, gravel, & coarse sands
Glaciers, mountain rivers, reefs, beaches
Intermediate energy environment
can carry grains such as sand & mud
Meandering rivers, delta, continental shelf & slope, deserts (dunes)
Low energy environment
carry fine sand, silt, & mud
River floodplains, tidal flats, continental shelf & slope, deep sea, deep lakes
Describe the 3 types of sedimentary rock and what they are classified by, also including examples of each rock.
Siliciclastic = forms from clasts of primarily silicate sediments
Classified by grain size & material of particles
sandstone
Biological = primary material is precipitated by microscopic organisms
classified by type of organic material & texture
chert, limestone
Chemical = precipitate from evaporation of water & deposited locally
Classified by chemical composition
Gypsum, Halite, Anhydrite
Where are all 3 types of sedimentary rocks formed?
passive continental margins, where there is an edge of a continent that is not a boundary
how do passive continental margins form?
Form by subsidence
Cooling of lithosphere after rifting
Weight of sediment pushes down surface of lithosphere
Transgression
landward movement of shoreline due to rising sea level or sinking of lithosphere (sea moves out more)
depositional environments move inland, leaving sedimentary deposits behind
Regression
seaward movement of shoreline due to falling sea level or rising continent (sea goes out)
depositional environments move seaward, forming layers of sediment
3 main factors in metamorphism
Change temp
Change pressure
Confining pressure (pressure due to weight of rocks)
Tectonic stress (applied force in particular direction)
Change fluid conditions
release/transport elements by fluids
Net results of metamorphism
Low P minerals transform into high P minerals; new minerals form with long axes parallel to minimum stress
Types of metamorphic changes
Change mineral composition
Change in texture
Change mineral type
Develop fabric (preferred orientation of minerals)
Foliation
Cleavage
Schistosity
Foliation
parallel alignment of platy minerals (such as mica or chlorite) in distinct layers or sheets from intense P and/or T
Cleavage (metamorphic)
tendency of certain minerals to break along foliation
Schistosity
type of foliation w/ metamorphic materials in wavy/wrinkled layers, where minerals grow in direction of minimum applied stress (since it is easiest)
When it comes to metamorphic changes, in general…
increasing _____ = increasing ______ size = enhanced ______ & _______ _______
grade
grain
schistosity
compositional banding
What are the 3 metamorphic grades in terms of pressure and temperature? What type of mineral is a cause of these grades?
Low grade - low P, low T
Intermediate - low P, high T OR high P, low T
High grade - high P, high T
Index minerals are diagnostic of metamorphic grade
The set of minerals in a metamorphic facies depends on…
the protolith (original rock type; igneous or sedimentary)
metamorphic minerals that grow depend on ______ composition
parent composition
different parents under same P-T conditions = different minerals!
actualism
physical processes that exist now also operated similarly in the past