-
scientific method
- observation
- hypothesis
- test; retest or revise
- peer review
-
Accretion
Assembling a large object by combining smaller fragments together.
-
How was moon formed
When earth was 70% of its current size it was hit by a mars size impactor.
-
Differentiation
Separation of materials based on density. Heavier materials settle out to bottom, lighter ones rise to top.
-
Layers that make up the earth's composition (chemical)
Crust, mantle, core
-
Layers that make up the earth's rheology?
Lithoshere, asthenosphere, mesosphere, inner core, outer core
-
Rheology
Material behaviors of the earth's structure, i.e., rigid or ductile
-
-
Isostasy
The rigid lithosphere floats on the ductile asthenosphere
-
2 types of lithosphere
Oceanic: thin and more dense & continental: thick and less dense
-
Hypothesis
Testable explanation for what you have observed
-
Density =
mass/volume. Or, how much/how big.
-
Gravity
Attractive force between masses
-
Radiation
Heat transfer due to light.
-
Convection
Heat transfer due to movement of material.
-
Conduction
Heat transfer due to contact.
-
Age of Earth
4.5 billion years old
-
Archemede's principle
An object will float if an equal amount of mass of the supporting fluid is displaced.
-
Isotope
Atoms of the same element that have different atomic masses. -- same # of protons but different # of neutrons
-
Atomic number
Number of protons in the nucleus. -- defines what element an atom is.
-
Atomic mass
Number of protons + number of neutrons
-
Atoms
The smallest unit of matter that has the properties of elements.
-
Ions
Atom with a charge imbalance. -- unequal # of protons and electrons.
-
Cation
Positively charged ion. -- more protons than electrons.
-
Anion
Negatively charged ion. -- more electrons than protons.
-
Valence shell
Outermost shell of electrons
-
Covalent bond
An atomic bond between atoms in which valence shell electrons are shared. -- strongest atomic bond. -- water
-
Ionic bond
An atomic bond formed by electrostatic attraction between ions of opposite charge when electrons are transferred. -- like NaCl, sodium chloride. -- two ions with opposite charge that hang out near eachother to appear charge balanced.
-
Metallic bond
An atomic bond where electrons are freely shared among nuclei.
-
Hydrogen bond
An atomic bond between the polar water molecule and other atoms/molecules.
-
Polar molecule
A molecule that has an equal number of protons and electrons but an uneven distribution of electrons across the molecule.
-
Van Der Waals
Weak static bonds.
-
types of plate tectonic boundries
- 1. convergent ==> <==
- [ocean-continent, ocean-ocean, continent-continent]
- 2. divergent <==>
- [mid-ocean ridge, continental rift]
- 3. transform ^ v [L.A. vs S.F.]
- plates rubbing against each other
-
3 types of subatomic particles
- protons (+)
- neutrons (+, -)
- electrons ( - )
-
atomic number
number of protons in the nucleus; define what element an atom is
-
5 special properties of H2O
- adhesion; attraction to other substances
- cohesion; attraction to other H2O molecules
- heat capacity; amount of energy that must be added/removed to change temperature
- expands when frozen
- universal solvent; really good dissolver
-
5 criteria for a mineral
- naturally occurring
- solid
- crystalline
- inorganic
- specific chemical composition
-
crystalline
atoms are arranged in a set repeating order
-
explain two ways to bond a tetrahedron into minerals
- glue using intermediate atoms (Fe, Mg)
- polymerize by sharing a neighboring tetrahedron's oxygen
-
silicate minerals (highest to lowest in density)
- olivine (100% glue)
- pyroxene
- amphibole
- mica
- feldspar
- quartz (100% polymerized)
-
silicate minerals tetrahedral arrangement (high to low density)
- isolated
- single-chain
- double-chain
- sheet
- 3D network
-
3 basic types of rocks
- igneous
- sedimentary
- metamorphic
-
igneous rock
rocks that are cooled/crystallized from a melt
-
sedimentary rock
assembled fragments of other rocks, or, precipitate dissolved minerals; break or dissolve
-
metamorphic rock
alteration occurs in a solid state; cook, squish, or soak
-
how to melt rocks
- raise temperature; breaks bonds
- lower pressure; increases space between atoms
- add H2O; molecular home-wrecker, lowers melting point
-
volcanic textures
- glassy; lava cooled too rapidly for crystals to form
- vesicular; magma cooled too rapidly for gases to escape
- pyroclastic; "fire" "fragment"; rock assembled from erupted material
-
viscosity
- measurement of a substance's resistance to flow
- high = thick, low = runny
-
volatiles of volcanology
- substances that are gases at magmatic temperatures
- H2O
- CO2
- form bubbles -- increase volume, lower viscosity
-
intrusive igneous environment
- cool slowly, deep underground
- cool using conduction
- plutonic
-
extrusive igneous environment
- cooled rapidly on the surface
- cools using radiation
- volcanic
-
aphanitic
- extrusive igneous texture
- very fine grained
- very small mineral crystals, need microscope to see
-
phaneritic
- intrusive igneous texture
- course grained
- minerals crystals seen with naked eye
-
pegmatitic
- intrusive igneous texture
- extremely course grained
- crystals > 1cm
-
porphyritic
- intrusive igneous texture
- large perfect mineral crystals surrounded by finer grained ground mass
- 2 stages of cooling
- chemical limits on crystal size (based on varied quantities of ingredients
-
six types of volcanoes
- continental caldera
- cinder cone
- flood basalt
- volcanic dome
- shield volcanos
- stratovolcano (or composite)
-
volcanic hazards
- ash fall
- ash flow
- mud flows (lahar)
- volcanic landslides
- tsunami
- lava flows
- gases
-
ash fall
- low particle : gas
- lower density, gas rich mixture
-
ash flow
- high particle : gas
- higher density
-
lahar
a sticky mixture of water and debris that is created when eruption products enter river channels or glaciers melt
-
volcanic gases
- CO2 + H2O ==> H2CO3 (carbonic acid)
- Lake Nyos, Cameroon
-
four signs of impending eruption
- seismicity; harmonic tremors -- small M1-M2 EQ that occur when magma intrude rocks
- gas emissions; seeping through soil from magma
- surface temperature; water temperature of springs and lakes
- surface deformation
-
weathering
breakdown of rocks by physical or chemical means
-
erosian
transport of materials
-
mechanical weathering
- the breakdown of rocks purely by physical means
- SA:V
- the more mechanically weathered a rock becomes, the more likely it is to weather further
-
six types of mechanical weathering
- frost wedging; water expands when frozen, exerts pressure on rocks
- crystal growth; water evaporates, leaves behind ions that form into crystals, exerting pressure on rocks
- mechanical exfoliation; rocks that form under pressure "peel apart" once the pressure is released
- tree roots and plants
- thermal expansion and contraction
- abrasion; rocks and sediment collide with eachother during transport
-
chemical weathering
- changes chemical composition of rocks and minerals
- converts unstable rocks and minerals on the earth's surface to stable ones
-
the role of H2O in chemical weathering
- carries ions to reactions
- participates in reactions
- carries reaction products away
-
three types of chemical weathering
- dissolution
- oxidation
- hydrolysis
-
chemical weathering by dissolution
- ions (or ion groups) are carried away by water
- example -- halite, NaCl -ionic bond
- example -- limestone is CaCO3; H2O + CO2 ==> H2CO3 (carbonic acid) H2CO3 dissolves limestone
-
chemical weathering by oxidation
- a mineral's ion combines with oxygen
- example -- Fe in mafic rocks
- example -- Fe2+ in minerals will oxidize to Fe2O3 (hematite) (rust)
-
chemical weathering by hydrolysis
- H+ or OH- ions from water displace other ions in a mineral structure
- example -- hydrogen bonding will break feldspars down into clay minerals
- the type of reaction that is used to break down certain polymers
-
3 types of sedimentary rocks
- detrital - broken fragments of other rocks
- chemical - previously dissolved minerals (crystalline)
- bioclastic - chunks of previously living organisms (bones, shells, teeth, etc.)
-
-
carrying capacity
- the volume of sediments that can be transported (how much)
- based on velocity; increase in V = increase in carrying capacity, decrease in V = deposition
-
competence
- the largest size sediment that can be transported (how big)
- based on velocity; increase in V = increase in competence, decrease in V = deposition
-
sedimentary sorting
- the separation of sediments based on size, shape and/or density
- poorly sorted, sorted, well sorted
-
lithification
- the process by which sediment becomes rock
- compaction or cementation
-
lithification by compaction
- pressure due to burial; overburdenoverlying pressure (weight) of sediments decreases volume, binding grains
-
lithostatic stress
- the pressure or stress imposed on a layer of soil or rock by the weight of overlying material
- pressure same in all directions
- squeezing out the empty spaces
-
lithification by cementation
- pore spaces (voids) will be filled in with cement minerals
- dissolved minerals precipitate out of solution and bind sediment grains
- calcium carbonate, silica, iron oxides
-
detrital classification
- based on grain size:
- boulder......
- gravel........
- pebble........ if angular = breccia; if rounded =conglomerate
- sand, sandstone
- mud, mudstone.......
- silt, siltstone..........
- clay, claystone........ if blocky or layered = shale
-
chemical classification
- based on composition and origin
- inorganic and biotic
-
classification of sedimentary structures
- bedding
- ripple marks
- mud cracks
-
four types of igneous textures
- aphanitic
- phaneritic
- pegmatitic
- porphyritic
-
bedding planes
- flat parallel layers of sediment
- caused by...
- changes in carrying capacity of the erosional agent
- changes in sediment composition
-
graded bedding
the sediment size decreases from the bottom of the bed to the top
-
cross-beds
- form due to dune processes
- the preserved slip faces found inside a dune
-
asymmetric ripples
ripples from a current moving in one direction
-
symmetric ripples
oscillation; current goes back and forth
-
mudcracks
records wet/dry cycles
-
metamorphism
- rocks are recrystallized in the solid state
- original features of the rock are altered or obliderated
-
protolith
parent rock; original rock before metamorphism
-
regional metamorphism
- large scale metamorphism due to tectonic processes
- burial
- subduction
- mountain building
- == more even distribution of changes
-
contact metamorphism
- small scale changes due to direct contact with agents of metamorphism
- igneous intrusions
- lava flows
- hydrothermal fluids
-
agents of metamorphism
- heat (temp)
- pressure (stress)
- fluids (H2O)
-
-
-
-
-
-
-
|
|