Set: Eosc 114 mass extinctions/earhquakes

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All 36 terms

TermDefinition
Biospherethin layer of life on earth's surface
Ordovician Oceanaround 450 Milion yrs BP
Cretaceous Oceanaround 130 million yrs BP
Principle of Superpositionwhat's on top is youngest
Principle of Faunal Successionstrata of like age can be recognized by the fossils they contain
Biostratigraphyusing the appearance and disappearance of fossils to subdivide geological time
Characteristics of mass extinctionat least 30% of species lost, broad range of ecologies, short/sudden
5 extinctions in Phanerozoiccretaceous/tertiary, end triassic, permo/triassic, late devonian, late ordovician
causes of mass extinctionsbiological, earth based, atmospheric, extraterrestrial, combination
Cretaceous/Tertiary Extinctiondinosaur killer, at least 50% species lost
The Crater: "the smoking gun"crater 180 km across off coast of Mexico, Chicxulub, asteroid 10 km across
Oort Cloudcomet store dirty snowballs, commonly around 15km diameter
Torino Scale0-10, assess risk of NEO
Proposed Mitigation Strategiesfragmentation, sudden orbit adjustment, steady state orbit adjustment, ablation system, ridind solar winds
3 types stressescompression, tension, transverse
faultlarge brittle fracture in a rock body, point of origin for most earthquakes, m-km
fracturesusually mm-cm
Reverse faultcaused by compression, block moves towards each other, hanging block moves upwards relative to footwall
Normal Faultcaused by tension, blocks move away, hanging wall block moves down relative to footwall
Hypocentre(focus) where motion begins on the fault
Epicentredirectly above the hypocentre on the surface
Elastic Rebound Theoryhow earthquakes build energy
Body WavesP and S waves, move within the Earth, much faster than surface waves, not damaging to buildings
P wavesprimary or pressure, fastest, travel through solids or fluids, arrive first (accordian)
S wavessecondary or shear, travel through solids only (slink)
Surface wavesvertical and horizontal waves, move at the surface, much slower than body waves, cause more damage (rayleigh, love)
Rayleigh Wavesup and down
Love Wavesside to side
Richter Scaleno longer in use, quantative scale, measures amplitude
Moment Magnitude Scalemeasures strain energy along rupture surface, logarithmic, each # 32x more energy releas and 10x more shaking
Foundation materialbedrock = more intense, well compacted sediment = less intense
Earthquake hazardsground shaking/ ground rupture, liquefaction, fire, tsunami, ground failure/landslide
Modified Mercali Scalequalitative measurement, what we feel, 1-12
divergent boundariessmaller earthquakes, associated with volcanoes
convergent boundariessmall to very large earthquakes, subduction zones are where largest volcanoes occur
tektitesproduced by melting rocks during impact

Set Information

Terms 36
Creator hkeller
Created April 25, 2009
Groups None
Subject natural disasters
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Most Missed Words

  1. Cretaceous/Tertiary Extinction dinosaur killer, at least 50% species lost - 4 misses
  2. Principle of Faunal Succession strata of like age can be recognized by the fossils they contain - 4 misses
  3. Biostratigraphy using the appearance and disappearance of fossils to subdivide geological time - 4 misses
  4. 3 types stresses compression, tension, transverse - 3 misses
  5. Cretaceous Ocean around 130 million yrs BP - 3 misses
  6. Elastic Rebound Theory how earthquakes build energy - 3 misses
  7. Ordovician Ocean around 450 Milion yrs BP - 3 misses