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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.