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Rocks Bellringer K= know about rocks already Rocks Bellringer K= know about rocks already

Rocks Bellringer K= know about rocks already - PowerPoint Presentation

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Rocks Bellringer K= know about rocks already - PPT Presentation

W Want to learn about rocks L Learned about rocks Rocks are composed of 1 or more minerals There are 3 types of rocks igneous sedimentary and metamorphic Rock cycle describes how the elements that make up rocks are redistributed transforming one rock into another ID: 634925

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Presentation Transcript

Slide1

RocksSlide2

Bellringer

K= know about rocks already

W= Want to learn about rocks

L= Learned about rocksSlide3

Rocks are composed of 1 or more minerals

There are 3 types of rocks: igneous, sedimentary, and metamorphic

Rock cycle describes how the elements that make up rocks are redistributed transforming one rock into anotherSlide4

4 parts of Earth

Inner core: mass of iron 7000 degrees Fahrenheit. Immense pressure keeps iron solid

Outer core: mass of molten iron. Electric currents produce Earth’s magnetic field

Mantle: slow moving molten rock or lava

Crust: sand and rockSlide5

Composition of Magma

Mix of molten rock, gases, and mineral crystals

Elements: O, Si, Al, Fe, Mg, Ca, K, Na

Compound most abundant: Silica

Silica content affects melting temperature and impacts how quickly magma flowsSlide6

Independent Work

Make a Venn Diagram comparing and contrasting minerals and rocks

Composition

Formation

Group

Elements PresentSlide7

Bellringer

Make a list of how you think rocks are used in everyday lifeSlide8

Magma Formation

Factors: temperature, pressure, water content, and mineral composition.

Temperature increases with depth in Earth’s crust

Pressure increases with depth. Due to weight of overlying rock

Small percentages of water are in rocks and minerals. Water content increases, melting point decrease.

Different minerals have different melting points. Slide9

Igneous Rock

Forms from crystallization of magma (molten rock below Earth’s surface)

2 types of igneous rocks

Extrusive: fine grained, cools quickly on Earth’s surface. Example: Rhyolite

Intrusive: coarse grained, cools slowly beneath Earth’s surface. Example: GraniteSlide10

Igneous Rock as a Resource

Useful as building materials

Interlocking grain= strength

Minerals in igneous rocks are resistant to weathering

Example: Granite

Ore depositsSlide11

Independent Work

1. What are the 2 different types of igneous rocks and describe how each forms?

2. What are the factors that affect the formation of magma?

3. Why do you think magma is usually a slushy mixture of crystals and rock.

4. Make a Frayer model: 1. 4 parts of the Earth. 2. How is magma formed. 3. Describe igneous rocks. 4. How can igneous rocks be used. Slide12

Bellringer

Make a list of things you know about fossilsSlide13

Sedimentary Rocks

Igneous rocks are the most common on Earth’s crust

Do not see igneous rocks on the ground

Earth’s surface is covered in sediments

Sediments= pieces of solid material that have been deposited on Earth’s surface by wind, water, ice, gravity, or chemical precipitation

Sediments cement together to form sedimentary rocks.

Formation begins with weathering and erosion. Slide14

Types of Sedimentary Rocks

Clastic

: Most common: Loose sediment: Varying sizes. Sandstone, shale

Chemical: Formed from evaporation. Limestone, Rock salt

Organic: Remains of once living things: Limestone, coalSlide15

Bellringer

Referring to last week’s KWL, make a list of things you have learned about rocks so far under “L”Slide16

Importance of Sedimentary Rocks

Form fossils: provide information about past animals and plants

Understand geologic change over time: flow of rivers, wave/wind directions, shorelines

Sources of oil, natural gas, and coal

Uranium mined from sandstone: nuclear power

Limestone: cement for constructionSlide17

Weathering

Weathering= physical and chemical processes that break rock into smaller pieces

Chemical weathering=rocks are dissolved or chemically changed

Physical weathering= minerals remain chemically unchanged. Rock fragments break off along fractures.Slide18

Illustrate the Rock Cycle

Terms to be used: igneous, metamorphic, sedimentary, magma, sediment, melting, heat, pressure, weathering, erosion, deposition, cementation, burial

Do not simply use the terms, you need a picture to show the process. You can refer to your rock cycle worksheet.

Slide19

Erosion and Transport

After rock fragments have been weathered, they are transported to a new location

Erosion- movement of surface materials from 1 location to another.

Agents of erosion= wind, moving water, gravity, and glaciers

Examples: muddy water, dust, fine sandSlide20

Deposition

Deposition= sediments are laid down on the ground or sink to bottom of bodies of water.

Sediment deposited when transport stops.

Fast-moving water can transport large particles.

As water slows, largest particles settle, then next-largest. Settles in layers

Wind moves small grains: Ex: sand dunes

Glaciers move all sizes easily: large boulders, sand, mudSlide21

Metamorphic Rock

Heat and pressure form metamorphic rocks

Heat: derived from Earth’s internal heat

Pressure: derived from vertical pressure by weight of overlying rocks or compressive forcesSlide22

Independent Work

Make a concept Map with Rocks in the middle.

From there, you need 3 legs for each of the types of rocks

Make bubbles for how formed, how used, examples, types.

Describe each further