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1.11 Sedimentary Bedding Structures

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    Hi guys,
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    the objective of this video is to look at
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    the bedding structures that form
    when sediment is deposited.
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    These bedding structures all form
    in different environments.
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    These environments which create the bedding
    structures will be discussed.
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    Firstly,
    we will talk about the horizontal beds,
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    or strata,
    that the sediment is laid down in.
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    Sedimentary rock is stratafied,
    which means that it has layers.
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    These layers have formed because sediment
    is laid down in horizontal layers called strata.
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    Between each layer of strata,
    we have bedding planes.
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    And these bedding planes form because
    the region has experienced
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    a change in depositional
    environment or material.
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    We can see here in this photo that we have
    had one type of sediment laid down.
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    And then,
    a change in depositional environment
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    has caused a different type of sediment
    to be laid down on top,
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    in between which is a bedding plane.
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    We know that the strata towards
    the bottom of a series is older
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    than the strata at the top.
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    And this happens because the sediment
    is laid in this way.
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    Bedforms are formations that occur due to
    the movement of wind and water.
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    Bedforms are created when water or wind,
    flows over loose sediment.
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    And the shape and the texture of the bedform,
    depends on the velocity of the flowing wind or water,
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    and the size of the sediment.
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    One type of bedform is ripples.
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    Ripples occur to due the flow of water.
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    Asymetrical ripples occur when water's
    just flowing in one direction.
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    As we can see here.
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    Symetrical ripples will occur
    when the waves oscillate back and forth.
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    As we can see here.
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    These bedforms can be preserved in
    the sedimentary rock,
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    because new sediment can be deposited on top.
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    And the formation will remain the same
    and will be lithified in this shape.
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    Another type of bedform are dunes.
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    Dunes form with the same formation process
    as the asymetrical ripples when they form
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    due to water.
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    However,
    dunes form due to the action of wind.
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    Cross Bedding is another type of
    bedform.
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    Cross bedding forms in the process of
    making ripples or dunes.
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    Whether that be with water or wind.
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    Cross bedding forms because we have
    a pile up of sediment along the top
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    of the slip face.
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    This pile up is being pushed
    towards the edge of the slip face
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    and soon will slip down the face.
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    This slip face will then slowly move
    downstream as more and more
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    sediment comes along.
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    Any additional sediment will continue
    to form cross bedded layers
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    in the environment where ripples and
    dunes are being formed.
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    Another type of bed form are
    graded beds.
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    Graded beds form when the
    strata of the sediment becomes
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    more fine towards the top of the strata.
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    This graded pattern is often repeated
    in a formation.
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    As we can see here.
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    Graded beds form due to a sudden period
    of high energy movement of the sediment.
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    For example,
    as we are actually discussed in the
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    previous video,
    graded beds will form when we have
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    turbidite cones;
    when sediment avalanches over
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    the edge of a continental shelf.
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    So,
    when the sediment avalanches over
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    the edge of the continental shelf,
    turbidite cones are created down here.
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    When the sediment is in the turbidite cone
    the heavy sediment will settle out first.
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    The medium size material will settle next,
    and the fine silt material will remain
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    suspended in the currents of the water,
    and will finally settle out on top.
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    This is what creates our graded beds.
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    The last thing we will discuss in this video are
    bed-surface markings.
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    Bed surface markings occur due to
    alterations on the surface of the Earth.
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    Mudcracks form when the surface of the
    Earth dries out.
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    Mudcracks can be preserved in the
    sedimentary layers when they are covered
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    by sediment.
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    These mudcracks indicate that we have had
    alternating wet and dry conditions
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    in the past.
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    Fossils are another type of bed surface
    marking.
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    Where fossils can be preserved within the
    layers of sediment,
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    and they are an evidence of past life.
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    In summary,
    sediment is laid down in horizontal beds.
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    We know these sedimentary layers can
    preserve past environments,
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    such as the flow of wind and water over
    loose sediment.
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    This flow of wind and water can create
    bedforms;
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    such as ripples, dunes and crossbedding.
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    And bed surface markings such as,
    mudcracks and fossils can also form
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    and indicate the environment in which
    the sediment was laid down in.
Title:
1.11 Sedimentary Bedding Structures
Description:

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Video Language:
English
Duration:
04:50

English subtitles

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