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Station One-Basalt

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Station One-Basalt (Write this description on your lab sheet) Basalt is one of the most common volcanic rocks. It is usually grey to black in color and fine-grained ... – PowerPoint PPT presentation

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Title: Station One-Basalt


1
Station One-Basalt
  • (Write this description on your lab sheet)
  • Basalt is one of the most common volcanic rocks.
    It is usually grey to black in color and
    fine-grained due to rapid cooling of the very
    fluid lava on the surface. Basalt is the
    principal rock of the ocean floor and is made up
    of feldspar and pyroxene.
  • Use the hand-lens to carefully look at this
    sample. Are you able to see any crystals? If so,
    describe them.
  • Using at least three adjective, describe the
    texture of this sample.

2
Station Two- Vesicular Basalt
  • (Write this on your lab sheet)
  • This specimen of Aye Aye lava is from Hawaii.
    This rock gets its name from the sharp points
    throughout its outer covering. When people walk
    barefoot on this rock they often yell Aye! Aye!
  • Describe how this rock MIGHT have cooled to form
    its sharp points.
  • 2. Look at the air bubbles in this sample.
    Do you think this rock cooled quickly or slowly?
    Explain your reasoning.

3
Station Three- Andesite
  • ( Write this on your lab sheet)
  • This igneous rock is a fine-grain rock that
    forms from lava flows from andesitic volcanoes.
    Andesitic volcanoes are often associated with
    subduction zones.
  • Use the loop to look at the crystals, then use
    the metric ruler to measure, in millimeters, the
    size of the largest crystal you can see.
  • Do you think this rock cooled quickly or slowly?
    Explain your thinking

4
Station Four-Obsidian
  • ( Write this on your lab sheet)
  • Obsidian is a naturally occurring volcanic glass
    formed a silica-rich volcanic rock. It is
    produced when lava, extruded from a volcano,
    cools quickly without crystal growth. Obsidian
    breaks with a very sharp fracture, which made it
    good for making cutting tools
  • 1. Describe how this igneous rock is different
    from other types.
  • 2. Describe the texture of the Obsidian?

5
Station Five- Hornblende Granite
  • (Write this on your lab sheet)
  • This igneous rock is coarse-grained, with
    equal-sized crystals, giving it an even texture.
    Hornsblende Granite is made up of Quartz,
    Feldspar, and Mica.
  • 1. Do you think this rock formed quickly or
    slowly? Would it be called intrusive or
    extrusive?
  • 2. Do you think this rock cooled quickly or
    slowly? Explain your reasoning.

6
Station Six-Granite
  • (Write this on your lab sheet)
  • Here are 2 specimens of Granite. Granite is the
    commonest of all intrusive igneous rocks. It can
    contain a variety of different minerals like
    Quartz, Feldspar, Mica, and Hornsblende.
  • 1. Describe the similarities and differences
    between these two specimens.
  • Are the crystals in each specimen the same size?
    What does that tell you about these specimens?

7
Station Seven-Scoria
  • (Write this description in your Rock book)
  • Scoria is a dark-colored, vesicular, extrusive
    igneous rock. The vesicles are a result of
    trapped gas within the melt at the time of
    solidification. It often forms as a frothy crust
    on the top of a lava flow or as material ejected
    from a volcanic vent and solidifying while
    airborne.
  • This volcanic rock appears to have various tan
    flecks within the black. Take a guess, how do
    you think it formed?
  • Describe the feel of this rock.

8
Station Eight-Pumice
  • (Write this description in your Rock book.)
  • Pumice is a light-colored vesicular igneous
    rock. It forms through very rapid solidification
    of a melt. The vesicular texture is a result of
    gas trapped in the melt at the time of
    solidification. Place the pumice in the container
    of water.
  • 1. Does this type of ROCK float or sink? Test
    it.
  • Study the texture and composition of this rock.
    Note all of the air bubbles that were present
    when this was a liquid are now just empty holes
    in the rock. Do you think this rock cooled
    quickly or slowing? Explain your thinking
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