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- Rocks are the most common material on Earth. They are naturally
occurring aggregates of one or more minerals.
- Rock divisions occur in three major
families based on how they formed: igneous, sedimentary, and metamorphic.
Each group contains a collection of rock types that differ from each
other on the basis of the size, shape, and arrangement of mineral
grains.
- The rock cycle is an illustration that is used to explain how the three
rock types are related to each other and how Earth processes change a
rock from one type to another through geologic time. Plate tectonic
movement is responsible for the recycling of rock materials and is the
driving force of the rock cycle
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- What are rocks:
- A mixture of minerals, mineraloids, glass, or organic matter
- Some rock forming minerals include feldspar, quartz, hornblende and
mica
- Granite is a mixture of feldspar, quartz, mica, hornblende, and other
minerals
- How are they mixed?
- Do they stay the same forever?
- Rock Cycle
- Cycle shows 3 types of rock and the processes that form them
- Throughout earth’s history, rocks of each type have been changed into
other types by natural forces
- Melting
- Cooling and hardening
- Weathering and erosion
- Compacting and cementing
- Heat and pressure
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- Sediments are particles that come from all rock types
- Carried by wind and water over thousands of miles
- Worn away rock is not destroyed rock
- Elements forming rocks and minerals not destroyed
- Only changes form
- Law of Conservation of Matter
- Changes in Rock Cycle don’t create or destroy
- Weathering processes break away existing rocks, even mountains
- Mineral matter broken away by wind, water, or ice but remains same
- Some mineral particles dissolve in streams and reacts with other
particles to form new minerals
- Chemical change
- New minerals may be different from original rocks and minerals
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- Igneous Rocks
- Formed from cooling magma
(molten rocks and minerals) or lava(magma that reaches earth’s surface)
- Quickly cooling lava forms extrusive or volcanic and have small mineral
grains
- Slowly cooling magma forms intrusive or plutonic and have large mineral
grains
- Sedimentary Rocks
- Sediment-pieces of rocks, minerals, organic remains and dissolved
minerals from water
- When sediment becomes solid it is sedimentary rock
- Sediment piles up on land, riverbeds, ocean floor and the layers build
up over time.
- Clastic, chemical, or organic sedimentary rocks form in different ways
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