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By:
 Maria
Andrade
   1. My first sample I
    collected was a
    igneous rock I
    identified as large
    Granite. Which is
    located just inside the
    entrance to Sequoia
    National Park also
    known as Tunnel Rock.
    This amazing park has
    been around since the
    Ice Age making this
    rock approximately
    20,000 years old.
   2. My second sample
    is a igneous rock I
    identified as large
    Granite. Which is
    located in Sequoia
    National Park.
    Granite rocks
    contain the mineral
    quarts and
    potassium feldspar.
    My favorite rock from
    all my samples.
   3. My third sample is
    a metamorphic rock
    that I picked up
    from Morro Bay. This
    rock contains
    Marble. This rock is
    very smooth and
    shows signs of
    metamorphism of
    limestone,
    composed mostly of
    calcite.
 4. My fourth sample is an
  igneous rock known as
  basalt. This is the most
  common type of
  igneous rock found on
  our planets upper crust.
  This sample came
  straight from my yard.
 What simplified my
  identification process
  was that the rocks
  texture was smooth
  textured, had straight
  fractures and dark color.
   5. My fifth and final
    example is a
    sedimentary rock that
    was created through
    cementation as
    percolating water
    coats the sediment
    with mineral matter,
    and gradually
    cements the particles
    together. This sample I
    found in the beach of
    Pismo.
   1. A fault that I
    observe was the San
    Andreas Fault. It runs
    on the California
    coast and into the
    to Mexican coast.
    This fault is a Strike
    fault exhibit mainly
    horizontal
    displacement
    parallel to the strike
    of the fault surface.
    2. An example of first example of
    weathering is mechanical weathering
    shown in the Sequoia Park. Mechanical
    weathering is accomplish by physical
    forces that break rock into smaller and
    smaller pieces without changing the
    rocks mineral composition. My second
    example is chemical weathering known
    in the second picture which shows the
    cave that is located in Pismo beach.
   3. The evidence that I got of mass
    wasting this stream which is located in
    Sequoia Park. Where slopes became
    overstepped and collapse. The
    evidence for erosion that I present is the
    beach of erosion. Erosion is caused by
    the incorporation of the transportation of
    material agent such as water.
   4. First for my continental sedimentary
    environment I have pictures of a stream
    in sequoia park. Second I have the
    transitional sedimentary environment of
    Pismo Beach. And thirdly the marine
    environment which can be found in the
    sea as turbidity currents.
Field
Field

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Field

  • 2. 1. My first sample I collected was a igneous rock I identified as large Granite. Which is located just inside the entrance to Sequoia National Park also known as Tunnel Rock. This amazing park has been around since the Ice Age making this rock approximately 20,000 years old.
  • 3. 2. My second sample is a igneous rock I identified as large Granite. Which is located in Sequoia National Park. Granite rocks contain the mineral quarts and potassium feldspar. My favorite rock from all my samples.
  • 4. 3. My third sample is a metamorphic rock that I picked up from Morro Bay. This rock contains Marble. This rock is very smooth and shows signs of metamorphism of limestone, composed mostly of calcite.
  • 5.  4. My fourth sample is an igneous rock known as basalt. This is the most common type of igneous rock found on our planets upper crust. This sample came straight from my yard.  What simplified my identification process was that the rocks texture was smooth textured, had straight fractures and dark color.
  • 6. 5. My fifth and final example is a sedimentary rock that was created through cementation as percolating water coats the sediment with mineral matter, and gradually cements the particles together. This sample I found in the beach of Pismo.
  • 7. 1. A fault that I observe was the San Andreas Fault. It runs on the California coast and into the to Mexican coast. This fault is a Strike fault exhibit mainly horizontal displacement parallel to the strike of the fault surface.
  • 8. 2. An example of first example of weathering is mechanical weathering shown in the Sequoia Park. Mechanical weathering is accomplish by physical forces that break rock into smaller and smaller pieces without changing the rocks mineral composition. My second example is chemical weathering known in the second picture which shows the cave that is located in Pismo beach.
  • 9.
  • 10. 3. The evidence that I got of mass wasting this stream which is located in Sequoia Park. Where slopes became overstepped and collapse. The evidence for erosion that I present is the beach of erosion. Erosion is caused by the incorporation of the transportation of material agent such as water.
  • 11.
  • 12. 4. First for my continental sedimentary environment I have pictures of a stream in sequoia park. Second I have the transitional sedimentary environment of Pismo Beach. And thirdly the marine environment which can be found in the sea as turbidity currents.