2 - Historical Geology Flashcards
study of changes to earth and life in time and space
historical geology
Types of ages
Relative time and absolute time
measurement of time using comparison methods
relative time
measurement of time using actual numbers
absolute time
how to measure earth’s relative age
by rock layer and faults
measuring earth’s absolute age
radioactive dating
half-life
the breaking down of atoms to form different isotopes of the same element or completely new element
radioactive dating
energy is given in the form of:
gamma rays, alpha particles, beta particles
the amount of time it takes for half of the original to decay
half-life
Fundamental theory
Uniformatarianism and catastrophism
same atomic number but diff atomic mass
isotope
who proposed the theory of uniformitarianism
james hutton 1785
TU: laws of nature are constant across time and space
Uniformity of law
TU:appropriate hypotheses
uniform of methodolgy
TU:past and present causes are all of the same kind
uniformity of kind
TU: geological circumstances have remained the same over time
uniformity of degree
popularized the catastrophism
Georges Cuvier 9th century
extinction event
formerly known as cretaceous tertiary k-t
Cretaceous-Paleogene
a large planetesimal somehow impacted the early earth, blew out rocky debris, remelted it and formed the moon
4.5 billion years ago
giant impact theory
distinct surface between two unlike bodies of rocks
contact
single layer or bed of rock
stratum
multiple layers of rocks
strata
study of strata
stratigraphy
a body of work with distinctive structure that is bounded by contacts
formation
locations or portions where rocks are exposed at the earth’s surface
outcrop/exposure
Fundamental principles pf historical geology formulated by nicolaus steno in 1669
superposition, original horizontality, lateral continuity, intrusive relationships, cross-cutting relationships
gaps in geologic record that may indicate episodes of crustal deformation, erosion and sea level variations
uncomformity
types of unconformities:
angular unconformities
disconformities and nonconformity
older package of sediments are tilted
angular conformity
lower package of sediments was not tilted prior to deposition of the upper sediment package
disconformity
separates igneous rocks from overlying sedimentary rocks
nonconformity
age of invertebrates
paleozoic era
age of dinosaurs and reptiles
mesozoic era
age of mammals
cenozoic era