ES Chap 5 & 6: Rocks

Similar documents
NOTE OUTLINE : Chap 5 & 6: Rocks

9/24/2017. ES Ch 5 & 6 Rocks 1. Objectives -Igneous. Chapters 5 and 6. Objectives - Sedimentary. Objectives Metamorphic. Objectives Rock Cycle

Chapters 5 and 6. Igneous, Sedimentary, and Metamorphic Rocks..

To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle

Igneous, Metamorphic & Sedimentary. Chapter 5 & Chapter 6

Name Class Date. Chapter 3 Rocks Chapter Test. Write the letter that best answers the question or completes the statement on the line provided.

Name Class Date. In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements.

A rock is a naturally occurring solid mixture of one or more minerals, or organic matter

Rocks. 3.1 The Rock Cycle. 3.1 The Rock Cycle. 3.1 The Rock Cycle. The Rock Cycle. I. Rocks

2 Igneous Rock. How do igneous rocks form? What factors affect the texture of igneous rock? BEFORE YOU READ. Rocks: Mineral Mixtures

Prentice Hall EARTH SCIENCE

Liz LaRosa Images from Geology.com unless otherwise noted

WHAT ARE ROCKS? ROCKS are a naturally occurring SOLID MIXTURE of one or more minerals and organic matter. Rocks are ALWAYS changing.

Rocks Rock- A group of minerals, glass, mineroid bound together in some way.

Chapter 10. Chapter Rocks and the Rock Cycle. Rocks. Section 1 Rocks and the Rock Cycle

THE ROCK CYCLE & ROCKS. Subtitle

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

2 Igneous Rock. How do igneous rocks form? What factors affect the texture of igneous rock? BEFORE YOU READ. Rocks: Mineral Mixtures

Earth Science Chapter 6 Rocks

IGNEOUS ROCKS. SECTION 5.1 What are igneous rocks?

IGNEOUS. What is a Rock? What is the difference between a rock and a mineral? Rocks are made up of minerals.

What is a Rock? Naturally-occurring mixtures of minerals, mineraloids, glass or organic matter.

6/20/2018. Lesson 1 (Properties of Minerals) 6 th Grade. Earth s Structure Chapter 2: Minerals and Rocks. density =

Rocks are made from Minerals

Chapter 9 : Rocks and Minerals

Rock Cycle. Presented by Kesler Science

Sedimentary Rocks Most common SURFACE rock

10/20/2015. How is magma different from lava? Magma is molten rock below the Earth s surface. Lava is magma that flows out onto Earth s surface.

I m good. Thank you.

Lecture 3 Rocks and the Rock Cycle Dr. Shwan Omar

Q. How do we know about the Earth s history? A. The ROCKS tell us stories

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

Topics that will be discussed


A Rock is A group of minerals that have been put together in several different ways.

Chapter 4 Rocks & Igneous Rocks

Rocks: Materials of the Solid Earth

I. Uniformitarianism- James Hutton s 2-part theory states: A. The geologic processes now at work were also active in the past B. The present physical

Igneous Rocks. Igneous Rocks - 1. Environment of Formation - Magma - Plutonic - rock that formed within the Earth. Intrusive - Earth s crust.

Page 1. Name: 1) Which diagram best shows the grain size of some common sedimentary rocks?

UNIT TOPICS TOPIC 1: MINERALS TOPIC 2: IGNEOUS ROCKS TOPIC 3: SEDIMENTARY ROCKS TOPIC 4: METAMORPHIC ROCKS TOPIC 5: THE ROCK CYCLE

Rocks. Geology: Slides 22-50

The 3 types of rocks:

Rocks & Minerals. Lesson 1 Properties of Minerals. What is a mineral? What is a mineral?

1. A solid material made up of one or more minerals or grains or other substances, including the remains of once-living things is a.

Minerals. What are minerals and how do we classify them?

Happy Tuesday. Pull out a ½ sheet of paper

CHAPTER ROCK WERE FORMED

Rock Types. Sedimentary Rocks. Lithification = becoming a rock

NAME: PERIOD: DATE: LAB PARTNERS: LAB #9 ROCK IDENTIFICATION

Name Class Date. 1. In your own words, write a definition for the term rock cycle.

S6E5: we will investigate the scientific view of how the earth s surface is formed. b. Investigate the contribution of minerals to rock composition

CHAPTER ROCK WERE FORMED

Which sample best shows the physical properties normally associated with regional metamorphism? (1) A (3) C (2) B (4) D

EES - Goal Rocks and Minerals

Earth and Space Science. Semester 2 Review, Part 2

ROCKS & MINERALS UNIT. 8 th Grade Earth & Space Science

Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock

The most common elements that make up minerals are oxygen, silicon, aluminum, iron, calcium, potassium, and magnesium

As compaction and cementation of these sediments eventually occur, which area will become siltstone? A) A B) B C) C D) D

BRYCE CANYON NATIONAL PARK Earth s Dynamic Treasures Rocks & The Rock Cycle

Structure of the Earth

Rocks and Minerals (rocksandminerals)

Minerals and Rocks. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left.

BELLRINGER QUESTION:

Rock Identification Lab, 60 Points This is a BIG lab! Work carefully and thoroughly

A. IGNEOUS Rocks formed by cooling and hardening of hot molten rock called magma (within crust or at its surface).

Rocks and The Rock Cycle

8 th Earth Science Chapter 4 Rocks Name Section 1 The Rock Cycle:

Review - Unit 2 - Rocks and Minerals

ROCK IDENTIFICATION LAB

TEACHER BACKGROUND KNOWEDGE. Minerals, Rocks and the Rock Cycle

Rock Cycle and Rock Types Homework

Rocks. Section 1:Igneous Rocks. Section 2:Sedimentary Rocks. Section 3: Metamorphic Rocks. Section 4: The Rock Cycle

Rock Identification. invisible rhyolite andesite basalt komatiite. visible granite diorite gabbro peridotite

Minerals By Patti Hutchison

Rocks and The Rock Cycle

The Rock Cycle The Rock Cycle illustrates the origin of igneous, sedimentary and metamorphic rocks

Rocks. Rock Cycle, Types of Rocks

COMPOSITIONAL TERMS: FELSIC : light colored INTERMEDIATE : medium shades MAFIC : dark colored ULTRAMAFIC : rare (composition of the mantle)

Rocks. Rocks are composed of 1 or more minerals. Rocks are classified based on how they formed (origin). 3 classes of rocks:

EARTH SCIENCE. Geology, the Environment and the Universe. Chapter 5: Igneous Rocks

PENNSYLVANIA. Ordinary processes at Earth's surface and just below it cause rocks to change and soils to form. Page 1 of 3. S8.A.1.1.

Compositional (Chemical) Layers

Chapter 6 Sedimentary and Metamorphic Rock

Version 1 Page 1 Barnard/George/Ward

* * * * *25

2-1 F. Objectives: Define rocks Describe the rock cycle and some changes that a rock could undergo.

transform boundary Photograph by Robert E. Wallace, USGS.

B) color B) Sediment must be compacted and cemented before it can change to sedimentary rock. D) igneous, metamorphic, and sedimentary rocks

Solid Earth materials:

Chapter Test C. Rocks: Mineral Mixtures MULTIPLE CHOICE

Instructor s Manual Chapter 3

Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100

Classify Rock (rock1)

Which rock is shown? A) slate B) dunite C) gneiss D) quartzite

Page 1. Name:

Minerals and Rocks. Test Review Activity. Begin

Hafeet mountain. Rocks

RR#7 - Multiple Choice

Transcription:

ES Chap 5 & 6: Rocks Objectives 1. Identify and explain characteristics of igneous rocks. This means that if I am given an igneous rock I: a. Can use grain size to identify a rock as intrusive, extrusive, or porphyry. In addition, I can discuss how the rate of cooling is related to grain size. b. Can use color to identify a rock as felsic, intermediate or mafic. c. Combining grain size and color (as described in a & b), I can use Table 5-2 on page 107 to name the rock. d. Use Table 5-2 page 107 to identify a rock if I am given the percent composition of a rock. i. Understand which minerals and rocks in Table 5-2 are high in silica, iron and magnesium. e. Discuss the factors that affect how rocks melt & crystallize f. Describe uses of igneous rocks. g. Rocks that may be samples to identify on the exam: obsidian, pumice, rhyolite, granite, basalt, gabbro. 2. Identify and explain characteristics of sedimentary rocks. This means that I: a. Can describe and list in order the steps that form clastic sedimentary rocks: Weathering (both physical and chemical), erosion, deposition, burial, lithification, cementation b. Can use information about ripple marks and fossils to infer what the past environment is like. c. Can identify a rock into one of the following subgroups; clastic, organic, chemical d. Can use the Law of Superposition to determine which rock layers are older or younger. e. Describe uses of sedimentary rocks. f. Explain miscellaneous terms such as porosity g. Rocks that may be samples to identify on the exam: conglomerate, breccias, sandstone, limestone, coal 3. Identify and explain characteristics of metamorphic. This means that I a. Can identify a rock into a metamorphic subgroup; foliated vs. non-foliated b. Explain the formation of metamorphic rocks. c. You will be asked to identify a rock as metamorphic and then as foliated or non-foliated, but you will not be asked to give it a specific name. 4. Understand how rocks continuously change from 1 type to another in the rock cycle. 5. I can identify a given rock sample into: a. One of the 3 main types of rock described above: igneous, sedimentary or metamorphic. b. Into the appropriate subgroup as described above. Sec 5.1 Classifying Igneous Rock 3 types of Rock: 1. Igneous: Formed from of a. Lava is magma that reaches & flows onto Earth s 2. Sedimentary: Formed from sediments together a. Sediments: Small pieces of 3. Metamorphic: Formed when a rock changes into a due to extreme ES Ch 5 & 6 Rocks Outline - 1-10/14/2012

Igneous Rocks: 1. Extrusive rocks: Fine ( ) grained rocks due to cooling on Earth s a. Examples: 2. Intrusive rocks: Coarse ( ) grained rocks due to cooling the surface Magma: a. Examples: The most common intrusive rock is 1. Composition: a. Mix of rock, gases, and mineral crystals b. Elements common in magma are the major elements found in Earth s crust: c. Most common compound: 2. Types: Based on the amount of Magma Type Amount SiO 2 Relative color of rocks when cools 1. Rhyolitic (Granitic) Special Characteristics 2. Andesitic 3. Basaltic 3. Origin: a. Heat of 800 1200 o C to b. This temperature is found in the and What heats the upper mantle & lower crust? c. Partial Melting is due to minerals with points i. Causes a slushy mix of rock & crystals Section 5.2 Classifying Igneous Rocks 3 Classifications of Igneous Rock: based on the of the rock 1. Felsic 2. Intermediate 3. Mafic ES Ch 5 & 6 Rocks Outline - 2-10/14/2012

Igneous rock type Type of Magma Silica (SiO 2 ) content Relative color Felsic Intermediate Mafic High in: Texture Rock Examples Extrusive Intrusive Main observations for igneous rock identification: 1. Color: vs. 2. Grain size: vs. Special IG rocks: 1. Porphyritic texture: Mixture of grains a. Complex cooling history: 2. Obsidian: Black glass 1. 1 st cooling deep in Earth-forming the crystals. 2. 2 nd cooling of remaining magma due to sudden or close to the surface a. Cooled that crystals are formed: 3. Pumice: 50% holes due to escape of trapped a. Formed from magma b. Used for abrasive polishing mixtures and cleansers Igneous Rocks as Resources 1. Building materials: & to weathering 2. Ore deposits: of substances within the rock a. Gold, silver, lead, & copper are not in compounds that form minerals, but they are found as ES Ch 5 & 6 Rocks Outline - 3-10/14/2012

b. c. Found in or i. Formed when liquid magma fills in other rocks & cools Sec 6.1 Formation of Sedimentary Rocks Steps to Form Sedimentary Rocks: 1. Weathering: Breaking down & of rocks into smaller pieces (called sediments which vary in size) a. Physical or mechanical causes of breakdown include: b. Chemical causes include of rocks by rain or chemicals 2. Erosion: of sediments to a new locations a. Possible means: 3. Deposition: or of sediments on the ground or bottom of bodies of water 4. Burial: Becomes beneath more & more sediments 5. Lithification: means making of and has 2 parts a. Compaction: Bottom layers of sediment are together by of upper sediment layers b. Cementation: Sediments are or together by minerals in the water that c. Summary: Lithification turns into Features of Sedimentary Rocks: 1. Layers (AKA beds) a. Law of : rocks on the if layers are undisturbed i. Exception occurs when layers are overturned by forces b. The following always form on the top of a layer. If they are found on the bottom instead, it indicates that layers have been overturned: 2. Sedimentary rocks usually form in 3. Sedimentary rock is rock on the (not in crust) of Earth a. Igneous rock is the most common rock in the CRUST, but it is buried. Most igneous rock is formed underground, not through lava on surface. ES Ch 5 & 6 Rocks Outline - 4-10/14/2012

Evidence of Past Life 1. Fossils: Preserved of once-living organisms a. Only found in rocks. WHY? b. During lithification, parts of organisms are replaced by & turned into rocks Sec 6.2 Types of Sedimentary Rocks 3 main groups of sedimentary rocks: 1. Clastic 2. Organic 3. Chemical Sedimentary Group Made from Subgroups & examples Clastic sedimentary rock 3 clastic subgroups based on grain size: 1. Coarse-grained: grains or larger a. Due to high water flows & speeds which can carry large pieces: 2. Medium-grained: -sized grains a. Form which has high porosity (incomplete cementation leaves between grains) b. Valuable reservoirs of 3. Fine-grained: a. Low porosity (barrier) Organic Examples: 1. Limestone: 2. : rock from buried swamp plants Chemical Example locations: 1. Coast of or the ES Ch 5 & 6 Rocks Outline - 5-10/14/2012

Importance of Sedimentary Rocks: 1. Fossils tell about a. Type of area and types of organisms: 2. tell the direction of in the past: a. Symmetrical ripple marks: i. Both sides of ripple have same shape ii. Indicates wave action b. Asymmetrical ripple marks: i. 1 side is gently sloped & other side is steep ii. Indicates wind or wave motion iii. Examples: 3. Energy a. b. Reservoir for when (open space) present 4. Limestone to make Sec 6.3 Metamorphic Rocks: rocks turned into a rock type Formation of Metamorphic Rocks 1. Pressure & temp with depth a. If hot enough to melt, rocks are formed b. If not hot enough to melt, but enough to change the rock, rock is made 2. Heat is due to or nearness to intrusions 3. Pressure is due to the pressure of of mountain building 4. Metamorphic rocks may be a. (alternate light & dark bands) due to with i. Lines may be straight or wavy ii. Example: Gneiss is formed from the igneous rock b. i. Example: Marble is formed from the sedimentary rock ES Ch 5 & 6 Rocks Outline - 6-10/14/2012

The Rock Cycle: 1. Is the of rock 2. Based on how new rock type is formed. 3. Following is an example of the possible changes the igneous rock granite could undergo. When it is: a. Weathered into new rock is formed b. Buried (but not melted) where affect it new rock is formed Comparison of the Characteristics of the 3 rock types: ES Ch 5 & 6 Rocks Outline - 7-10/14/2012

Computer Review: http://www.glencoe.com/sec/science/earthscience/index.html a. Chapter Resources b. Unit 2 c. Chapter 5 and Chapter 6 Diagram-Igneous Intrusions #2 ES Ch 5 & 6 Rocks Outline -8-10/14/2012

WS: Rock Record, Figure #1 WS: Rock Record, Figure #2 WS: Rock Record, Figure #3 ES Ch 5 & 6 Rocks Outline - 9-10/14/2012

WS: Rock Record, Multiple Choice Figure ES Ch 5 & 6 Rocks Outline - 10-10/14/2012