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*The following words and
information are from rocksforkids.com
The Rock Cycle
Rocks are constantly being formed, worn down and
then formed again. This is known as the rock cycle. It is like
the water cycle but it takes a lot longer. It takes thousands
and millions of years for rocks to change.
Rocks
are divided into 3 types:
(1) Igneous
(2) Sedimentary
(3) Metamorphic
What
category a rock is in depends on how the rock was formed.
Igneous
Rocks
Igneous means made from fire
or heat. When volcanoes erupt and the liquid rock comes up to
the earth's surface, then new igneous rock is made. When the
rock is liquid and inside the earth, it is called magma. When
the magma gets hard inside the crust, it turns into granite.
Most mountains are made of granite. It cools very slowly and is
very hard.
When
the magma gets up to the surface and flows out, like what
happens when a volcano erupts, then the liquid is called lava.
Lava flows down the sides of the volcano. When it cools &
turns hard it is called obsidian, lava rock or pumice -
depending on what it looks like.
- Igneous
rocks form when molten lava or magma cools and turn to solid
rock. The magma comes from the Earth's core which is
molten rock. The core makes up about 30% of the Total
Earth Mass (31.5%)
- There
are 5 kinds of igneous rocks, depending on the mix of
minerals in the rocks.
Granite contains quartz, feldspar & mica
Diorite contains feldspar & one or more dark
mineral. Feldspar is dominant.
Gabbro contains feldspar & one or more dark
mineral. The dark minerals are dominant.
Periodotite contains iron and is black or dark.
Pegmatite is a coarse-grained granite with large crystals of
quartz, feldspar and mica
- Obsidian
is nature's glass. It forms when lava cools quickly on
the surface. It is glassy and smooth.
- Pumice
is full of air pockets that were trapped when the lava
cooled when it frothed out onto the surface. It is the
only rock that floats.
Sedimentary Rocks
When mountains are first
formed, they are tall and jagged like the Rocky Mountains on the
west coast of North America. Over time (millions of years)
mountains become old mountains like the Appalachian Mountains on
the east coast of the United States. When they are old, they are
rounded and much lower. What happens in the meantime is that
lots of rock gets worn away due to erosion. Rain, freeze/thaw
cycle, wind and running water cause the big mountains to crumble
a little bit at a time.
Eventually most of the broken
bits of the rock end up in the streams & rivers that flow
down from the mountains. These little bits of rock & sand
are called sediments. When the water slows down enough, these
sediments settle to the bottom of the lake or oceans they run
into. Over many years, layers of different rock bits settle at
the bottom of lakes and oceans.
Think of each layer as a page
in a book. One piece of paper is not heavy. But a stack of
telephone books is very heavy & would squish anything that
was underneath. Over time the layers of sand and mud at the
bottom of lakes & oceans turned into rocks. These are called
Sedimentary rocks.
Some examples of sedimentary
rocks are sandstone and shale.
Sedimentary
rocks have fossils in them because plants & animals that
have died get covered up by new layers of sediment and are
turned into stone. Most of the fossils we find are of plants
& animals that lived in the sea. They just settled to the
bottom. Other plants & animals died in swamps, marshes or at
the edge of lakes and were covered with sediments when the size
of the lake got bigger.
When large amounts of plants
are deposited in sedimentary rocks, then they turn into carbon,
which gives us our coal, oil, natural gas and petroleum. A large
sea once covered the central part of Canada and the climate was
very tropical. In time, sedimentary rocks formed there. That is
why we find dinosaur fossils in Alberta and the area is a good
source of natural fuels.
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Sedimentary
rocks cover 75% of the earth’s surface. Most of the
rocks found on the Earth’s surface is sedimentary even
though sedimentary rocks only make up less than 5% of all
the rocks that make up Earth.
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When
rocks are exposed to the elements – air, rain, sun,
freeze/thaw cycle, plants – erosion occurs and the
little bits of rock worn away get deposited as sediments.
Over time, these sediments harden as they get buried by
more sediments and turn into sedimentary rocks.
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Sedimentary
rocks are usually formed in layers (strata).
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There
are 6 main kinds of sedimentary rocks depending on the
appearance of the rock.
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Conglomerate
rock has rounded rocks (pebbles, boulders) cemented
together in a matrix.
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Sandstone
is a soft stone that is made when sand grains cement
together. Sometimes the sandstone is deposited in layers
of different coloured sand.
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Shale
is clay that has been hardened and turned into rock. It
often breaks apart in large flat sections.
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Limestone
is a rock that contains many fossils and is made of
calcium carbonate &/or microscopic shells.
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Gypsum,
common salt or Epsom salt is found where sea water
precipitates the salt as the water evaporates.
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Porphory
rock is when jagged bits of rock are cemented together in
a matrix.
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Metamorphic Rocks
Metamorphic rocks are rocks
that have changed. The word comes from the Greek
"meta" and "morph" which means to change
form. Metamorphic rocks were originally igneous or sedimentary,
but due to movement of the earth's crust, were changed.
If you squeeze your hands
together very hard, you will feel heat and pressure. When the
earth's crust moves, it causes rocks to get squeezed so hard
that the heat causes the rock to change. Marble is an example of
a sedimentary rock that has been changed into a metamorphic
rock.
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Metamorphic
rocks are the least common of the 3 kinds of rocks.
Metamorphic rocks are igneous or sedimentary rocks that
have been transformed by great heat or pressure.
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Foliated
metamorphic rocks have layers, or banding.
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Slate
is transformed shale. It splits into smooth slabs.
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Schist
is the most common metamorphic rock. Mica is the most
common mineral.
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Gneiss
has a streaky look because of alternating layers of
minerals.
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Non-foliated
metamorphic rocks are not layered.
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Marble
is transformed limestone.
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Quartzite
is very hard.
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