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L.O: By the end of this lesson I will be able to explain the cyclical processes within rock cycle. ESRT Page-6

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ESRT pg 6

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Do now: in “Upco”, read pages 67- 68.

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- Shows how rocks change from one type to another because of the interactions with water, air, and land.

The Rock Cycle

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Earth’s rocks are constantly changing from one form to another. They are constantly:

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THE ROCK CYCLE SHOWS 3 THINGS

  • NEARLY ALL ROCKS ARE

MADE FROM OTHER ROCKS.

  • ROCKS ARE CLASSIFIED

ON THE BASIS OF THEIR ORIGIN

  • THERE ARE A VARIETY

OF WAYS A ROCK CAN

CHANGE, IT JUST DEPENDS

ON THE ROCKS ENVIRONMENT.

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Important Vocabulary

Weathering – is a process in which rocks are physically and chemically broken down by water, air, and living things.

Erosion - transportation of material.

Deposition - When an agent of erosion (water, wind, ice, or gravity) lose energy and sediments drop back to the ground

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Important Vocabulary

Magma – is molten material that forms deep beneath the Earth’s surface.

Lava – Magma that reaches the surface.

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Internal Energy

Processes driven by heat from Earth’s interior are responsible for forming both igneous and metamorphic rocks.

Energy for the rock cycle comes from

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External Energy

Weathering and the movement of weathered materials are external processes powered by energy from the sun & produce sedimentary rocks.

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On the earth science regents:�

You will have to identify the class of three rocks.

(is it igneous, sedimentary or metamorphic) and describe its properties.

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Let’s Review

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Sedimentary Rocks

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Metamorphic Rocks

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Things to look for to help you identify an igneous rock

  • Vesicles /gas pocket holes (in pumice, scoria, vesicular basalt.)
  • Glassy texture. (obsidian)
  • The rock contains obviously intergrown crystals. (granite)
  • Contains large crystals (pegmatite)

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If it has vesicles (gas pockets),

It is igneous!

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Vesicles = an igneous rock

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A Vesicular rock on Mars, so Mars Has volcanoes!

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If it has a black glassy texture,

Its an IGNEOUS ROCK!

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IF IT HAS OBVIOUS INTERGROWN CRYSTALS

(LIKE THIS GRANITE), ITS IGNEOUS!

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OBVIOUSLY LARGE CRYSTALS = IGNEOUS

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LARGE CRYSTALS = IGNEOUS

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OBVIOUS STRATIFICATION (LAYERS) =

SEDIMENTARY ROCK (SANDSTONE)

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If it looks like pieces cemented together, its

A sedimentary rock.

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If you see fossils, shells, or the remains of

once living things, its sedimentary!

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If you see foliation (mineral alignment, its metamorphic

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If you see banding,(thick mineral alignment), its metamorphic

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If the rock looks distorted, its metamorphic

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Exit Reflection

Under what conditions can one rock change into another?

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Independent Work

  • Identify the given rocks.