unit 4 Flashcards
core
inner = solid, outer = liquid, mostly composed of iron
mantle
82% of earth’s volume and 67% of earth’s mass, asthenosphere, iron, silica, magnesium, oxygen
asthenosphere
“plastic rock”, outer molten layer, allows for plate movement
crust
outermost and thinnest layer, continental crust = 29% of earth’s surface, oceanic crust = 71% of eath’s surface
earth’s internal processes
gravity, convection currents, mantle plumes, heat from earth (deforms mantle so it flows)
heat from earth’s core
mantle deforms and flows, plates constantly move, convection cells, mantle plumes
convection cells
large “bubbles” of heated rock move
mantle plumes
molten rocks travel up a column, spread in radial pattern near crust
where can earthquakes and volcanoes b e found
along belts, at hot spots, or at plate boundaries
ring of fire
pacific plate boundary
lithosphere
outer shell, 20 plates, made of crustal rock and part of upper mantle
alfred wegener 1915 continental drift
continents were connected in a super continent (Pangaea) but they broke apart and drifted
evidence of continental drift
matching fossils found in africa and south america, mountains with similar structure, age, and mineral composition, ancient climates
pangaea
supercontinent, broke off into Laurasia and Gondwanaland
divergeant boundary
plates move in OPPOSITE directions, upwelling of material from mantle “sea-floor spreading”, newest land is closest to boundary
convergeant boundary
plates move together, destroying crust, subduction occurs
subduction
oceanic crust is denser than continental crust so it sinks under continental
oceanic-continental convergeance
oceanic and continental crust collide, ocean plate sinks below, plate melts and magma flows up = volcanoes, trench formation
oceanic-oceanic convergeance
oceanic crust collides from both directions, formation of volcanoes, trench formation
continental continental convergeance
continental crust collides from both directions, forms highest mountains in the world
transform boundary
plates grind past one another without producing or destroying crust, NO volcanoe formation
hot spot
usually hot area in mantle layer
hawaiin hot spot
pacific plates move past northwest at 9 cm per year, hot spot doesn’t move with plate = chain of volcanic islands produced
earthquake
vibration of earth produced by rapid release of potential energy caused by plate slipping along a fault
fault
large fracture in earth’s crust
surface waves
slowest, travel along earth’s outer layer, all other vibrations of seismogram
body waves
primary and secondary
primary body waves
travel through solids, liquids, and gases, 1.7 times faster than s-waves
secondary body waves
travel ONLY through solids
p waves on seismogram
first markings because they travel the fastest
s waves on seismogram
first larger waves
richter scale
measures wave amplitude and energy
time travel graph
used to see how far an earthquake traveled, looks at difference in arrival times of P and S waves
wave amplitude
each number is a 10x wave amplitude increase
wave energy
30x energy increase between each level
primary effects of earthquake
shaking, ground displacement
secondary effects of earthquake
rockslides, subsidence, fires, flooding, tsunamis, roads destroyedsoil liquefaction
Anak Krakatau
most powerful volcanic erruption in recorded history, located west of sumatra in indonesia
where do we find volcanoes
divergeant boundaries, convergeant boundaries, hot spots
magma
hot, molten rock that forms beneath earth’s surface
lava
molten rock that reached earth’s surface through volcanic vents
what’s inside magma
silica = determines viscosity (flow resistance)
what decides how violent a volcanic erruption is
temperature, silica composition, amount of gases dissolved; greater pressure = greater violence
affect of temperature on volcanic violence
temp increases = more energy in magma, dissolved gasses move faster, more collisions occur and pressure increases
affect of amount of gases dissolved on volcanic violence
more gases dissolved = more collisions in magma chamber, greater pressure
shield volcanoes
large volcanoes with gently sloping sides, made of liquid lava, usually occur at hotspots, less violent erruptions, shorter time between erruptions, lower viscosity
cinder cone volcanoes
small volcanoes with steep sides, frequently occur in groups, made of pyroclastic material
pyroclastic material
hot gas and volcanic solid fragments ejected during volcanic erruption
composite volcano
fromed by alternating layers of lava and rock fragments, tallest and most violent types, most common, “ring of fire”
cryptodome
part of volcano sinks in, sign that erruption will soon occur
after volcanic erruption
gases remain in atmosphere and go into clouds, cloud droplets reflect suns energy and help to cool the planet
soil
thin covering over most land
factors that affect soil formation
parent rock/material, time, climate, biota, soil food web, slope/topography, weathering
climate
most influential on soil formation, CO2 + water = carbonic acid in soil, temp affected decay rate, precip affects weathering