do now what is a rock? why do you think rocks look different?

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Do Now • What is a rock? • Why do you think rocks look different?

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Page 1: Do Now What is a rock? Why do you think rocks look different?

Do Now

• What is a rock?• Why do you think rocks look different?

Page 2: Do Now What is a rock? Why do you think rocks look different?
Page 3: Do Now What is a rock? Why do you think rocks look different?

Objective

I will be able to describe how igneous, sedimentary and metamorphic rocks are formed.

Page 4: Do Now What is a rock? Why do you think rocks look different?

Rock Cycle Video

Page 5: Do Now What is a rock? Why do you think rocks look different?

Types of Rock

Page 6: Do Now What is a rock? Why do you think rocks look different?

Sedimentary Rock Formation

• Sedimentary rocks are formed from loose pieces of sediment and sand which are pressed and cemented together; The layers get squashed together.

Page 7: Do Now What is a rock? Why do you think rocks look different?

Sedimentary Rock Vocabulary

Page 8: Do Now What is a rock? Why do you think rocks look different?

Sediments- broken rock materials; may also contain plant and animal matter.

Page 9: Do Now What is a rock? Why do you think rocks look different?

Weathering- the breakdown of rock by wind and water.

Erosion-is the transporting of the broken rock material, or sediments, to a new location, where it is deposited.

Page 10: Do Now What is a rock? Why do you think rocks look different?

Compaction- process where the upper layers put pressure on the lower layers causing small sediments to stick together

Page 11: Do Now What is a rock? Why do you think rocks look different?

Cementation- a solution of minerals and water seeps between large sediments and "glues" them together.

Page 12: Do Now What is a rock? Why do you think rocks look different?

Sedimentary Rock Characteristics

• Flat or curved layers• Particle size may be the same or

vary • Usually has pores between

pieces

Page 13: Do Now What is a rock? Why do you think rocks look different?

Sandstone, Limestone, Shale, Conglomerate

Page 14: Do Now What is a rock? Why do you think rocks look different?

Metamorphic Rock Formation

• Metamorphic rock is formed from preexisting rocks when heat, pressure and stress cause cause the rock to melt and turn into magma.

Page 15: Do Now What is a rock? Why do you think rocks look different?

Metamorphic Rock Vocabulary

• Metamorphosis- "change" or "transformation". • Magma is melted rock trapped

beneath the Earth's surface. • Lava is magma that has reached

the Earth's surface.

Page 16: Do Now What is a rock? Why do you think rocks look different?

Metamorphic Rock Characteristics

• Can be formed from igneous rocks, sedimentary rocks, or other metamorphic rocks.

• May have alternate bands of light and dark minerals

• Rarely has pores or openings

Page 17: Do Now What is a rock? Why do you think rocks look different?

Gneiss, Marble, Quartzite, Slate

Page 18: Do Now What is a rock? Why do you think rocks look different?

Igneous Rock Formation

• Igneous rocks form when magma or lava cools and hardens.

Page 19: Do Now What is a rock? Why do you think rocks look different?

Igneous Rock Vocabulary

• Extrusive- Igneous rock that forms above the Earth's surface. • Intrusive- Igneous rock that forms

below the Earth's surface.

Page 20: Do Now What is a rock? Why do you think rocks look different?

Igneous Rock Characteristics

• Normally contains no fossils • Usually made of two or more minerals • May be light or dark colored • May be fine-grained or glassy (extrusive)

Page 21: Do Now What is a rock? Why do you think rocks look different?

Granite, Basalt, Obsidian

Page 22: Do Now What is a rock? Why do you think rocks look different?

Rock Cycle Journey

• Worksheet• Comic Strip

Page 23: Do Now What is a rock? Why do you think rocks look different?

Objective

I will be able to describe how igneous, sedimentary and metamorphic rocks are formed.

Page 24: Do Now What is a rock? Why do you think rocks look different?

Rock Cycle

Page 25: Do Now What is a rock? Why do you think rocks look different?

Do Now

• Take out your Homework and place it on the front edge of the table.

• What is the rock cycle?

Page 26: Do Now What is a rock? Why do you think rocks look different?
Page 27: Do Now What is a rock? Why do you think rocks look different?

Objective

I will be able to describe the rock cycle.

Page 28: Do Now What is a rock? Why do you think rocks look different?

Igneous Rock Crystallization

• When it cools slowly it forms coarse-grained rocks.

• When it cools fast if forms fine-grained rocks.

http://www.classzone.com/books/earth_science/terc/content/investigations/es0603/es0603page05.cfm

Page 29: Do Now What is a rock? Why do you think rocks look different?

Rock Cycle Graphic Organizer

Page 30: Do Now What is a rock? Why do you think rocks look different?

Turn it over and write the following on the back

The Rock Cycle is a process that builds, destroys and changes the

rocks in the crust.

Page 31: Do Now What is a rock? Why do you think rocks look different?

Where do the rock cycle facts go?

Wind + water (weathering) = breakdown rocks

Page 32: Do Now What is a rock? Why do you think rocks look different?

Broken Rocks + plant & animal matter = sediment

Page 33: Do Now What is a rock? Why do you think rocks look different?

Pre-existing rock + heat and pressure = melted rocks

Page 34: Do Now What is a rock? Why do you think rocks look different?

Small sediments + pressure of upper layers = compaction

Page 35: Do Now What is a rock? Why do you think rocks look different?

Lava Cools and Hardens = Extrusive Rock

Page 36: Do Now What is a rock? Why do you think rocks look different?

Broken rocks + deposited at new location= erosion

Page 37: Do Now What is a rock? Why do you think rocks look different?

Large sediments are glued together = cementation.

Page 38: Do Now What is a rock? Why do you think rocks look different?

Quick Cooling Magma = Fine-grained rocks

Page 39: Do Now What is a rock? Why do you think rocks look different?

Slow Cooling Magma = Coarse-grained rocks

Page 40: Do Now What is a rock? Why do you think rocks look different?

Magma Cools and Hardens = Intrusive Rock

Page 41: Do Now What is a rock? Why do you think rocks look different?

Exit Ticket

• How are sedimentary rocks formed?• How are metamorphic rocks formed?• How are igneous rocks formed?

Page 42: Do Now What is a rock? Why do you think rocks look different?

Do Now

• What are minerals?• Where do you think you could find minerals in

nature?

Page 43: Do Now What is a rock? Why do you think rocks look different?
Page 44: Do Now What is a rock? Why do you think rocks look different?

Rocks and Minerals

Page 45: Do Now What is a rock? Why do you think rocks look different?

Rocks and Minerals Graphic Organizer

Page 46: Do Now What is a rock? Why do you think rocks look different?

Minerals Video

Page 47: Do Now What is a rock? Why do you think rocks look different?

Characteristics of Minerals

1. Must be a solid2. Must occur in nature3. Chemical composition4. Crystalline structure5. Must be inorganic

Page 48: Do Now What is a rock? Why do you think rocks look different?

Characteristics of Rocks

1. Mixtures of different types of minerals2. May contain organic materials3. Many rocks are not solid (magma)4. Naturally occurring

Page 49: Do Now What is a rock? Why do you think rocks look different?

Rock/Mineral Data Table

Sample ColorTexture (Fine or Coarse)

Shiny or Dull

Smooth or Rough

Looks like glass or metal

Size (in. or cm.)

Rock Group (igneous, metamorphic, sedimentary)

Mineral?

Page 50: Do Now What is a rock? Why do you think rocks look different?

Analyze and Conclude

• Use your samples and table to answer the following questions.

• Which of the samples could be a mineral? What physical properties do they share with the other samples? How are they different?

• What properties were most useful in classifying the samples? Why?

Page 51: Do Now What is a rock? Why do you think rocks look different?

Exit Ticket

• How are rocks and minerals different?