Exam 3 Flashcards
layers of rock at the bottom are usually older than the layers above them
Superposition
sedimentary layers usually start out flat and stay flat until they are deformed
Horizontality
fossils are found in the same order that the creatures lived on Earth
Fossil Succession
crystalline rocks underlay younger sediments, with a gap in time between them
Nonconformity
deformed rocks underlay flat rocks, with a gap in time between them
Angular unconformity
flat rocks underlay flat rocks, with a gap in time between them
Disconformity
younger rocks or faults cut through older ones
Cross-Cutting
older rocks can be trapped as pieces inside younger rocks
Included Pieces
versions of the same element (same protons) but different atomic weights (different neutrons)
Isotope
unstable and radioactive isotope which will decay over time
Parent element
new element created by the decay of the parent, builds up over time
Daughter element
the time it takes for half of the parent element to turn into daughter element.
Half life
dating system useful very young rocks, fossils, and archeological items. Must be organic
Carbon-14
dating system useful for very old rocks
Uranium-238
time of planetary formation, water added from volcanoes and comets. Life begins.
Hadean Eon
no oxygen in air, life remains primitive. First photosynthesis
Archean Eon
oxygen builds up in air, first ozone layer, life becomes more complex.
Proterozoic Eon
age of fish, first hard fossils, first trees and insects, life moves on land
Paleozoic Era
age of dinosaurs
Mesozoic Era
age of mammals
Cenozoic Era
stretching at divergent boundaries (rifting, spreading)
Extensional stress
crunching at convergent boundaries (subduction, collision)
Compressional stress
slicing at transform boundaries
Shear stress
temporary flexing, stores energy
Elastic strain
permanent slow bending, releases energy gradually
Ductile strain
permanent break, releases energy violently and suddenly
Brittle strain
vibrations in rock caused by released energy
Seismic waves
underground location where the fault actually breaks
Focus
surface map location above the focus
Epicenter
move fast by compressing rocks, can travel in solids or liquids
Primary (P) waves
move more slowly by slicing rocks, can only travel in solids
Secondary (S) waves
slowest and most damaging, make the ground surface move
Surface (L) waves