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- (Set up for Cornell Notes)
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- Rocks are made of a mixture of minerals & other materials video
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- Formed from lava or magma (Both are molten or liquid rock)
- Magma= underground
- Lava = above ground
- 2 basic types of igneous rock
- Intrusive/Plutonic– form when magma cools
- Large crystals (coarse-grained)
- Extrusive/Volcanic– form when lava cools
- Small crystals (fine-grained)
- Think: Why are the crystal sizes different?
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- Rocks form from magma cooling beneath Earth’s surface
- Takes a long time to cool and harden
- Coarse (large) grained
- Crystals form and grow (granite)
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- Rocks crystallize from cooling magma
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- Forms from magma that is brought to Earths surface (lava)
- Lava cools more rapidly so crystals do not have time to form or are
small and difficult to see
- Fine grained or lacking crystals like Obsidian
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- Yes. But they are still classified as intrusive or extrusive.
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- Yes. But they are still classified as intrusive or extrusive.
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- Formed from compressed (squeezed)
or cemented layers of sediment
- There are 3 types
- Clastic – formed from mechanical weathering debris or pieces of other
rocks that are glued together. (ex. Sandstone)
- Chemical – formed by precipitation of different elements dissolved in
water.
- Organic – formed from remains of
living things
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- Like soil or dirt, they are products of weathering that form at or near
Earth’s surface.
- Weather or nature is the major factor here. For example:
- Water
- Rivers cutting through
- Ice
- Rain
- Earthquakes
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- The rock is formed from weathered debris that is carried from one place
to another, redeposited, buried, and then hardened into rock.
- Sediments are compressed from the weight above the forming rock.
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- Rocks that contain fossils are sedimentary rock.
- Why will you only find fossils in sedimentary rock?
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- A rock that forms from other rocks as a result of intense heat,
pressure, or chemical processes.
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- Animation! http://www.classzone.com/books/earth_science/terc/content/investigations/es0602/es0602page02.cfm
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- Fossils are usually found in sedimentary rocks
- Paleontologists are scientists who study fossils
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- Petrified: minerals replace tissue of dead/buried organism
- Mold: hollow impression left by an organism
- Cast: copy of organism’s shape (fits the mold)
- Carbon film: thin layer of carbon left by organism (looks like a
drawing)
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- Trace Fossil: fossilized evidence of an organism’s activities
- Preserved remains: remains of life w/little or no change
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- Fossils help scientists understand how the Earth’s climate, environment,
and life forms have changed through time
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- Relative age is a comparison.
“older” and “younger”
- Absolute age is a number.
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- Law of superposition: In horiz. layers of sed. rocks, the oldest layer
is at the bottom, and higher layers are younger than the layers beneath
them.
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- Igneous intrusions are always younger than the layers of rock that
surround them
- Index fossils tell the relative age of the rock layer they are found in
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- Scientists use the rate of radioactive decay to determine the absolute
age of an igneous rock layer
- (Why only igneous?)
- Radioactive decay has been used to determine that the Earth is at least
4.6 billion years old
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- Word List
- Igneous Rock
- Intrusive
- Extrusive
- Fine Grained
- Silica
- Course Grained
- Magma
- Lava
- Light Colored
- Dark Colored
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- Word List
- Clastic
- Chemical
- Organic
- Precipitation
- Sediment
- Water
- Ice
- Earthquakes
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