Geol

Cards (100)

  • Deep Time
    the immense span of geologic time
  • James Hutton was called...
    the father of modern geology
  • Who was the first to articulate the "principle of uniformitarianism"?
    James Hutton
  • What is James Hutton's principle of uniformitarianism?

    "The present is the key to the past"
  • What are the 2 ways to date geologic materials
    relative ages, numerical ages
  • Relative age
    based upon order of formation, determination of older vs. younger relationships, developed hundreds of years ago
  • Numerical ages
    actual number of years since an event, developed recently.
  • Who created a set of principles for deciphering earth history?
    Sir Charles Lyell
  • The principle of uniformitarianism
    processes observed today were the same in the past
  • Principle of Original Horizontality
    Sediments settle out of a fluid by gravity.
  • Tilted sedimentary rocks are _______.
    deformed
  • The principle of superposition
    Younger strata are on top and older strata on bottom
  • The principle of lateral continuity.
    Subsequent erosion dissects once-continous layers
  • the principle of cross-cutting relations

    Younger features cut across older features
  • principle of baked contacts
    a igneous intrusion cooks the invaded country rock. The baked rock must have been there first (it is older).
  • Principle of Inclusions (rock fragments within another)
    Inclusions are always older than the enclosing material.
  • Physical principles allow us to
    sort out relative age even in complex situations.
  • Fossils are preserved in ________ rocks.
    sedimentary
  • Fossils are ____ _____ for relative age-dating.
    time markers
  • First _________, _________, and _______ are used for dating
    appearance, range, extinction.
  • Fossil Range
    the first and last appearance, each fossil has a unique range
  • ______ fossils are diagnostic to a geologic time.

    index
  • Unconformity
    a time gap in the rock record from erosion and non deposition.
  • an unconformity is a time gap in the rock record from
    erosion and nondeposition
  • 3 types of unconformity
    angular, nonconformity, disconformity
  • what does angular unconformity represent
    a huge gulf in time. Horizontal at first, new mountain range, eroded mountains, new horizontal layers.
  • Angular unconformity process

    Horizontal layers first, then a mountain range formed and eroded, then new horizontal layers form on top.
  • nonconformity
    igneous/metamorphic rocks capped by sedimentary rocks.
  • nonconformity process
    igneous or metamorphic rocks were exposed by erosion, sediment was deposited on the eroded surface.
  • Disconformity
    parallel strata bounding nondeposition. Often hard to recognize
  • Disconformity process
    An interruption in sedimentation, pause in deposition, sea level falls then rises, erosion
  • Eons
    the largest subdivision of time, not consistent number
  • Eras
    subdivisions of an eon
  • Periods
    subdivisions of an era
  • epochs
    subdivisions of a period
  • Phanerozoic (Eon)

    visible life
  • Proterozoic Eon
    before life
  • Archean eon

    ancient
  • hadean eon
    hell
  • Cenozoic era
    "recent life"