Term
|
Definition
|
-meteorite impats
-one killed the dinosaurs
-generate heat and impact
|
|
|
Term
|
Definition
|
-hot magma chamber
-high temperature
-low pressure
|
|
|
Term
|
Definition
|
-rocks slide across each other
-cold rocks-fault breccia (broken)
-hot rocks- flow to make mylonite
|
|
|
Term
| Hydrothermal Metamorphism |
|
Definition
|
|
Term
|
Definition
|
-continent-continent collision
-cold near surface, hot deeper down
-low temp/low pressure
-high temp/high pressure
|
|
|
Term
| Subduction Zone Metamorphism |
|
Definition
|
-low temp/high pressure
-slab is cold, takes a while to heat up
|
|
|
Term
|
Definition
|
-sedimentary rocks deposited younger over older
|
|
|
Term
| Law of Original Horizonality |
|
Definition
|
sediments deposited in horizontal beds
|
|
|
Term
| Law of Cross-Cutting Relations |
|
Definition
|
-younger features transect older ones
-light-colored granitic dike cuts older, banded metamorphic rock
|
|
|
Term
| Inclusions
(Relative Age Dating) |
|
Definition
|
-Older material encolosed within younger
igneous, sedimentary, or metamorphic
|
|
|
Term
| Angular Uncomformities
Uncomformities
(Relative Age Dating) |
|
Definition
|
-sedimentary rock over tilted/folded/eroded strata (sedimentary rock)
|
|
|
Term
| Disconformity
Uncomformities
(Relative Age Dating) |
|
Definition
|
-sedimentary rock over emergence and erosion (sedimentary rock)
|
|
|
Term
| Noncomformity
Uncomformities
(Relative Age Dating) |
|
Definition
|
-sedimentary rock over eroded igneous rock (had intruded sedimentary rock)
|
|
|
Term
|
Definition
|
-gives definate interval of geologic time
-fossils appear in geologic record in a definite order
-based on succession of fossils found in vertical sequences of sedimentary rocks
|
|
|
Term
| Dendrochronology
(Tree-Ring dating)
Absolute dates |
|
Definition
|
measurement of annual ring widths at tree heights
|
|
|
Term
|
Definition
|
-different number of neutrons
-frequently used in radiometric dating
|
|
|
Term
| Alpha Decay
(Radioactive Decay) |
|
Definition
|
-alpha particle emission
-lower atomic number and atomic mass
-lose an atom
|
|
|
Term
| Beta decay
(Radioactive Decay) |
|
Definition
|
-beta (electron) emission
-higher atomic number
-same atomic mass
-neutron transforms into electron
|
|
|
Term
| Electron Capture
(Radioactive Decay) |
|
Definition
|
-electron capture
-lower atomic number
-same atomic mass
-electron into neutron
|
|
|
Term
|
Definition
|
constant rate-> half-life
|
|
|
Term
| Radiometric Dating of Rocks
conditions |
|
Definition
|
-CLOSED SYSTEM (no parent or daughter leaves the rock)
-different teperatures
|
|
|
Term
| Igneous
Radiometric Date Meaning |
|
Definition
|
-time since crystallization from magma
|
|
|
Term
| Metamorphic
Radiometric Date Meaning |
|
Definition
|
time since metamorphism or recrystallization
|
|
|
Term
| Sedimentary
Radiomentry Date Meaning |
|
Definition
|
not closed (water in it)
age of clasts
|
|
|
Term
| Marine Magnetic Anomalies |
|
Definition
|
-magenetic reversals of seafloor spreading
-calibrated by radiometrically dated lavas on land
|
|
|
Term
|
Definition
|
-oldest rocks
-4030 million years old
|
|
|
Term
|
Definition
|
-3.8 to 2.5 million years ago
-reducing atmosphere-little oxygen,
-toxic to most current life
-continental plates began to form
-stromatolites abundant
|
|
|
Term
| Hamelin pool stromatolites |
|
Definition
|
-oldest organisms on earth
-fossils 3.5 billion years ago
-formed by single-cell organism: cyanobacteria
|
|
|
Term
|
Definition
|
-2.5-1.8 billion years ago
-oxygen (waste product of plants) banded with abundant dissolved iron to yield minerals like magnetite and hematite
-amount of oxygen locked up in banded iron beds-20x volume of oxygen in atmosphere today
-important source of iron ore
|
|
|
Term
|
Definition
|
-2.5 billion to 543 million years ago
-stable continents appear and acrete
-first abundant fossils of living organisms (bacteria and archaenas)
|
|
|
Term
| Prokaryotes vs. eukaryotes |
|
Definition
|
-pro-dna organized in single chromosome, no nucleus, no mitosis
-euk-dna organized in multiple chromosomes inside a nucleus, mitotic division
|
|
|
Term
|
Definition
|
-late proterozoic era fossil
-found on underside of course sandstone/mudstone- suggests a rapid burial
-worldwide presence
-not found after onslought of mineralized organisms in Cambrian period
|
|
|
Term
|
Definition
|
-time when Earth must have been covered by a sheet of ice
-rapid greenhouse warming from carbon dioxide took Earth out of icy tomb
-repeated cycle
-abundant co2 held in limestones
-led to proliferation of animals
|
|
|
Term
|
Definition
|
Age of Invertebrates, Fish, Amphibians
|
|
|
Term
|
Definition
|
|
Term
|
Definition
|
Age of Mammals, humans develop
|
|
|
Term
|
Definition
|
-general term for changes in volume or shape of rock masses in response to applied forces
-caused mainly by gravity
|
|
|
Term
|
Definition
|
-CAUSE of deformation
-force applied to volumes of rock
|
|
|
Term
|
Definition
|
EFFECT of deformation resulting from applied stresses
|
|
|
Term
|
Definition
|
-same in all directions
-simply pressure
|
|
|
Term
|
Definition
|
|
Term
| Hydrostatic Stress
(type of Uniform Stress) |
|
Definition
|
like on the bottom of a swimming pool
|
|
|
Term
| Lithostatic stress
(type of Uniform STress) |
|
Definition
|
"felt" by rocks deep in the earth from overburden and surrounding rocks
|
|
|
Term
| Normal Stress
(type of Differential Stress) |
|
Definition
|
directed perpendicular to surfaces
|
|
|
Term
| Shear Stress
(type of Differential Stress) |
|
Definition
|
directed parallel to surfaces, causing sliding
|
|
|
Term
| Compressional Stress
(type of Differential Stress) |
|
Definition
|
directed inward, leads to shortening of rock
|
|
|
Term
| Tensional Stress
(type of Differential Stress |
|
Definition
|
directed outward and can lead to stretching of rock
|
|
|
Term
| types of changes from STRAIN |
|
Definition
|
-length changes
-volume changes
-angular changes: between lines; surfaces sliding past one another
|
|
|
Term
|
Definition
|
-resistance to deformation
-function of pressure and depth- the deeper in the Earth, the stronger the rocks
|
|
|
Term
|
Definition
|
completely and instantly recoverable
|
|
|
Term
|
Definition
|
-creates sharp discontinuities
-when rocks pushed beyond elastic limit
(ie earthquakes)
|
|
|
Term
| Ductile (Plastic) Deformation |
|
Definition
|
-continuous deformation
-begins at critical strength:YIELD STRENGTH
-strength of ductile material governed by composition, temp, rate of deformation
-strength lower for greater T or lower strain
|
|
|
Term
|
Definition
|
-where deformations take place on Earth
-marked by earthquakes and surface deformation
-plate boundaries: ridges, subduction zones, and transfrom faults where plates pull apart, converge and slide past another can result in extreme thinning or thickening of the crust
|
|
|
Term
| Strike
to define a plane in space
-to describe faults and folds |
|
Definition
|
compass direction in horizontal plane
|
|
|
Term
| Dip
to define a plane in space
-to describe faults and folds |
|
Definition
|
-inclination of plane normal to strike
in the vertical plane
-max inclination of the plane
|
|
|
Term
| Joints
(example of Crustal Deformation) |
|
Definition
|
-cracks/fractures in rock with little/no visible displacement
-common-exploited by weathering
-commonly in parallel arrays or networks
-(alligned squares)
|
|
|
Term
| Faults
(example of Crustal Deformation) |
|
Definition
|
-fractures with obvious displacement
-common-shallow crustal deformation
-classified according to direction of displacement (and strain)
-(shifted/displaced squares)
|
|
|
Term
| Divergence
(example of Crustal Deformation) |
|
Definition
|
-vertical compression from gravity
results in horizontal extension
-example of divergent boundary-oceanic ridges
-oceanic crust made at the ridge
-lithosphere thickens and subsides as it cools
|
|
|
Term
| What happens with a normal fault? |
|
Definition
|
-before- nice horizontal layers
-small offset- hanging wall drops down relative to footwall
-large offset- active fault, hanging wall sliding downwards
-erosion- fault line scarp
|
|
|
Term
| Convergence
(example of Crustal Deformation) |
|
Definition
|
-horizontal compression
-results in horizontal shortening
-examples:
-Thurst Fault: hanging wall moves UP relative to foot wall
-older rocks move over younger rocks
|
|
|
Term
|
Definition
|
collision of India and Asia
|
|
|
Term
| Surface features along a strike-slip fault |
|
Definition
|
-rocks move past each other horizontally
-stand on one side of fault surface, see where the other side moves to determine which type of lateral strike-slip fault it is
-drainage offets
-linear valley along fault
-active and inactive fault traces
|
|
|
Term
| Folds
(example of Crustal Deformation) |
|
Definition
|
-tilted and bent rock layers
-caused by layer-parallel shortening
-common-deeper level crustal deformation
-classified by shape/geometry
|
|
|
Term
|
Definition
|
2 sandstones incline away from each other
|
|
|
Term
|
Definition
|
-2 sandstones folding the same direction together
-big "U" shape
|
|
|
Term
|
Definition
|
-N-S and E-W folding
-circular area where strata pushed up relative to what's around it
-hot targets for oil/gas
-exposed by erosion- younger rocks on outside, bottom
|
|
|
Term
|
Definition
|
-N-S and E-W folding
-rocks in center pushed down relative to what's around them
-Older rocks on the outside, top
|
|
|
Term
|
Definition
|
-weak ones from volcanoes
-strong- motion along faults, disconnect between rocks on either side of the fault, motions occur and release energy
|
|
|
Term
| Elastic Rebound Theory
(Earthquakes) |
|
Definition
|
-Earthquake- elastic rebound of previously stored elastic strain energy in the rocks on either side of the fault
-energy released is based on how much slick there is, how much rocks aredeformed, over how much area the fault moved
|
|
|
Term
| p-waves
(generated by earthquake)
(body wave-travel through earth) |
|
Definition
|
-compressional waves
-horizontal pressure
-~6km/s FASTER than S waves
-SLOWER in liquids than in solids
|
|
|
Term
| s-waves
(generated by earthquake)
(body wave-travel through earth) |
|
Definition
|
-shear waves
-diagonal pressure
-3.5 km/s
-slower than P waves
-can ONLY travel through solid
|
|
|
Term
| Raleigh waves
(generated by earthquake)
(surface wave) |
|
Definition
|
|
Term
| love waves
(generated by earthquake)
(surface wave) |
|
Definition
|
|
Term
|
Definition
|
-P-waves arrive first (travel faster)
-then S-waves
-then surface waves
|
|
|
Term
|
Definition
|
-3 seismic stations
-triangulation
|
|
|
Term
|
Definition
|
-meaure of the degree of earthquake shaking at a given locale
-based on the amount of damage
-scale: I-XII
|
|
|
Term
|
Definition
|
-Estimates the amount of energy released at the source of the earthquake
-large eq: 9
-based on amplitude of the largest seismic wave recorded (p or s)
-RMS of 2 is 10 times greater than RMS of 1
|
|
|
Term
|
Definition
|
-log(amplitude) + (distance correction)
distance correction is time difference between P and S wave arrival
|
|
|
Term
| First Motion of an earthquake
versus an atomic bomb |
|
Definition
|
-distinct quadrants of push or pull
versus all regions experiencing an initial push away from epicenter
|
|
|
Term
| large earthquakes to fewer occur on... |
|
Definition
|
-subduction zones (Alaska, Japan)
-collision zones (Himalayas by India/Asia)
-(both on convergent plate boundaries)
-strike-slip plate boundaries on land (SF)
-divergent plate boundaries (East African Rift)
|
|
|
Term
| the most subduction occurs in |
|
Definition
|
|
Term
|
Definition
|
-from EQ shaking
-caused large slope failure
-cracks develop in crust
|
|
|
Term
|
Definition
|
-Earthquake waves in the sea
-low amplitude (increases rapidly as seafloor shallows and speed and wavelength decrease)
-long wavelength
|
|
|
Term
| Earthquake prediction
short-term (hours, days, weeks) |
|
Definition
|
-based on precursor changes
-uplift/subsidence of land surface
periods of renewed/reduced minor seismicity
-changes in gasses emitted from wells
-abnormal animal behavior
|
|
|
Term
| long term earthquake prediction (years, decades, centuries) |
|
Definition
|
-based on probabilities
-risk assessment maps based on historical data
-seismic "gaps" :buildup of strain along plate boundary
|
|
|
Term
| Seismology
(geophysics-indirect investigations) |
|
Definition
|
tells:
-earthquake: location, strength, physical properties, movements
-seismic refraction
-seismic reflection
|
|
|
Term
| magnetism
(geophysics-indirect investigations) |
|
Definition
|
-tells core dynamics, paleomagnetics (plate motions, reversals, etc)
-mass flow
|
|
|
Term
| heat flow
(geophysics-indirect investigations) |
|
Definition
|
tells convection/conduction, lithosphere thickness
|
|
|
Term
| gravity
(geophysics-indirect investigations) |
|
Definition
|
density distributions near surface
|
|
|
Term
| seismic refraction
Seismology
(geophysics-indirect investigations) |
|
Definition
|
velocity, physical properties, layer thinknesses
|
|
|
Term
| seismic reflection
Seismology
(geophysics-indirect investigations) |
|
Definition
|
-internal gemoetry
-waves bouncing off earth
-mapping the subsurface (under ocean or inside the earth)
|
|
|
Term
| Seismic Tomography
Seismology
(geophysics-indirect investigations) |
|
Definition
|
|
Term
| velocity of compressional waves (p-waves) |
|
Definition
|
higher velocity in higher density
|
|
|
Term
|
Definition
|
-bending-path bends away from normal to interface with increasing density (and velocity)
-travel more where you can travel quickly so biggest angle in highest density
increase velocity with increase depth- waves move faster inside Earth
|
|
|
Term
| liquid outer core proved by: |
|
Definition
|
-P and S wave shadow zone
-P waves refracted off liquid and placed constraints on radius of liquid core
-S waves ended at liquid
|
|
|
Term
|
Definition
|
seperation between liquid outer core and and solid inner core
|
|
|
Term
|
Definition
|
-seismic discontinuity of increasing P wave velocity with depth
-boundary between crust and uppermost mantle (within lithosphere)
|
|
|
Term
|
Definition
|
-thin (5-7 km)
-dense (basaltic)
-mostly young (<200 my old)
|
|
|
Term
|
Definition
|
-thick (20-70 km)
-less dense (granitic)
-mostly very old (<4500 my old)
|
|
|
Term
|
Definition
|
-thermal boundary layer
-includes crust and part of upper mantle
-thickness depends on temp (thin where hot and young)
|
|
|
Term
|
Definition
|
-hot, weak part of upper mantle
-solid, but weak relative to lithosphere
-NOT molten, may have melt in it
|
|
|
Term
|
Definition
|
-strong lower part of mantle
-solid like lithosphere
-650-2800 depth
|
|
|
Term
|
Definition
|
-without any transfer of mass
from radioactive decay in Earth's interior (near surface in granitic material)
-higher in young, thin lithosphere and areas of active magmatism
|
|
|
Term
|
Definition
|
-heat because movement of mass/water
-movement of magma from mantle to surface
-seafloor spreading (formation/recycling of plates)
hydrothermal circulation (black smoker, geysers, etc.)
|
|
|
Term
| important mechanism of cooling the Earth |
|
Definition
|
generation of new oceanic lithosphere and recycling by plate tectonics- large scale convection of the planet
|
|
|
Term
| conductive cooling of lithosphere causes |
|
Definition
|
-lithosphere-asthenosphere boundary move down at rate proportional to:
1/(age of lithosphere)^2
|
|
|
Term
|
Definition
|
function of matter and motion in the Earth's magnetic outer core
|
|
|
Term
|
Definition
|
show age of strips of oceanic crust worldwide
|
|
|
Term
|
Definition
|
G(m1 x m2)/r^2
-m1=measuring device
-m2=mass between device and center of Earth
|
|
|
Term
|
Definition
|
-negative=mass deficiency
-positive=mass excess
-show how actual gravity field differs from gravity of uniform/featureless Earth
|
|
|
Term
|
Definition
|
-determine bathymetry based upon slight changes in elevation of sea surface from greater gravitational attraction of large rock masses on sea floor (volcanoes)
|
|
|
Term
| to learn topography of seafloor |
|
Definition
|
-echo-sounding
-swath mapping
-satellite altimetry
|
|
|
Term
| to learn geology of ocean floor |
|
Definition
|
-side-scan sonar (reflectivity of sound signal)
-ROVs (remotely operated vehicles)
-Alvin (submersible)
-Ocean drilling program
|
|
|
Term
| Passive continental margin |
|
Definition
|
-margin (where continental crust transitions into oceanic crust) created by spreading at mid-ocean ridge
-WEST coast of South America
|
|
|
Term
| Active continental margin |
|
Definition
|
-margin (where continental crust transitions into oceanic crust) adjacent to a subduction zone (or strike-slip boundary)
-contains oceanic trench
-EAST coast of US
|
|
|
Term
| Continental shelf
on Passive continental margin |
|
Definition
|
-submerged extension of CONTINENT
-nearly horizontal
-thick
-(during Ice Age, was exposed)
|
|
|
Term
| continental slope
on Passive continental margin |
|
Definition
|
-seaward edge shelf
-steeper
-boundary between continental/oceanic crust
|
|
|
Term
| continental rise
on Passive continental margin |
|
Definition
|
-more gradual slope
-very wide (merges into abyssal plain)
-thick with sediments from continental slope
-turbidity currents make deep sea fans
|
|
|
Term
|
Definition
|
-deep ocean trenches
-~11 km below sea level
|
|
|
Term
| terrigenous
on ocean basin floor |
|
Definition
|
-derived from land-mineral grains from continental rocks
|
|
|
Term
| biogenic
on ocean basin floor |
|
Definition
|
derived from organisms- marine animal shells, organisms
|
|
|
Term
| precipitates
on ocean basin floor |
|
Definition
|
derived from water- minerals crystallize out of water
|
|
|
Term
|
Definition
|
may occupy as much as 1/3 of ocean basin
|
|
|
Term
|
Definition
|
long-lived, large volcanic features that are randomly distributed through the ocean basins (and on land)
|
|
|
Term
|
Definition
|
-smaller volcanoes that erupt commonly near the ridge axis
-generally, do not rise to sea surface
|
|
|
Term
|
Definition
|
marine structures composed mainly of coral (some live but mostly dead skeleton) and some algae and sediment
|
|
|
Term
|
Definition
|
-colonies of coral generally near the shore
-require warm temperature, clear sunlit water, and nutrients from ocean water
|
|
|
Term
|
Definition
|
-circular coral structure with an interior lagoon
-can be >1000 m thick
|
|
|
Term
|
Definition
|
-area of high elevation
-belt of HIGHLY DEFORMED rocks resulting from contractional thickening and uplift of the crust
-thickening and uplift expose deep level metamorphic and igneous rocks
|
|
|
Term
| Andean type
of Orogenic/Mountain Belt |
|
Definition
|
-magmatic arcs above subduction zones
-accreted terrains "smeared" onto them during subduction
-Foreland basins of sedimentary rocks
|
|
|
Term
| Collisional Type
of Orogenic/Mountain Belt |
|
Definition
|
collided continental margins-at least one was a subduction zone (possibly both)
suture zone marks seam where 2 continents welded together
remnants of Andean type typically found
|
|
|
Term
|
Definition
|
collage of old continental fragments and orogenic belts
old "cratons" are rifted and surrounded by somewhat younger orogenic belts
|
|
|
Term
| Wilson Cycle
Major Earth Process |
|
Definition
|
oceans open and close
-rifting and continental margin development
-seafloor spreading
-subduction
-collision
-continued convergence
-new cycle...
|
|
|
Term
|
Definition
|
horizontal stretching, crust/lithosphere thinning, subsidence, sedimentation (burial)
*good sedimentary record, but deep rocks not exposed
|
|
|
Term
|
Definition
|
horizontal shortening, uplift, crust/lithosphere thickening, erosion (exhumation)
*sedimentary record deposite far away, surface material removed and deep level rocks exposed
|
|
|
Term
|
Definition
|
rifted continental margin
once a rift and spreading center, not a plane interior
|
|
|
Term
|
Definition
|
marks the site of a former oceanic tract
|
|
|