Timeline (MYA = Million Years Ago) Our Earth is 4.5 billion years old. Slide 1. Chapter 2. Slide 2. Slide 3
|
|
- Morgan Griffith
- 7 years ago
- Views:
Transcription
1 1 Chapter 2 2 The Mood According to geologists, for millions of years Utah Land was covered by warm, shallow seas teaming with small shelled animals, fish, and then reptiles. The seas came and went over and over again. During this time our oil, gas, and coal were being formed. The seas dried and sand covered the land. Dinosaurs lived here for millions of years. Then mammals, including giant mammoths and musk ox, came. Eventually mountains and plateaus were formed. Volcanoes erupted, bringing copper, gold, and silver from deep in the earth. The Ice Age cooled things off and caused glaciers to form. When the air finally warmed, melted ice formed a deep lake. People eventually came, living on what the ever-changing land provided. 3 Timeline (MYA = Million Years Ago) Our Earth is 4.5 billion years old 4.5 BYA to 600 MYA Precambrian Era (85% of the earth s time period) MYA Paleozoic Era (Shallow seas cover Utah.) Trilobites, amphibians, reptiles live in seas. Limestone, oil, gas, salt, potash, shale are in rock MYA Mesozoic Era (Dinosaurs and primitive mammals appear.) Shallow seas, then sandy deserts cover the land. Sedimentary rock of Utah s national parks is formed. River system exists. Dinosaurs disappear. 65 MYA Present Cenozoic Era (Mammals live here.) Mountains are formed. Plateaus rise. Volcanoes erupt. Copper and other minerals occur in rock. Carving of Canyonlands begins. Ice Age glaciers blanket northern Utah mountains. Lake Bonneville covers much of Utah, then declines. Great Salt Lake gets saltier. Humans appear.
2 4 5 6 Shaping the Land We know about Utah s Geography, but do you know how it came to be? What is the name of scientists who study the land, its formations, and rocks? Geologists Geo = Rock ology = The study of In Utah, we can see many things that tell us how our land has been shaped. Geologic Eras Precambrian era almost nothing living during this time about 85% of all the Earth s billion years falls within this era The oldest rocks of the continents formed during this time Paleozoic era Paleo means ancient Zoic means life This era produced the beginnings of the fossil fuels we have today (coal, oil, and natural gas). Geologic Eras continued Mesozoic era Meso means middle Zoic means life This era is associated with dinosaurs (In Utah, bones have been found in Jensen, Vernal and Price). The Rocky Mountains began to take shape during this era. Cenozoic era Ceno means recent Zoic means life In this era, the Earth began to be shaped similar to how we see it today. Giant mammals replaced dinosaurs during this era. Several ice ages changed the layout of the land, creating the Great Lakes, and Lake Bonneville. Human beings lived here at the end of this period.
3 7 Ancient Seas and Sandstorms. Sedimentary Rock covers much of Utah. Sediment loose sands, shells, and pebbles. Forming Sedimentary Rock Sediments are forced together over time forming a hard layer of rock. As time passes and more sediments are forced together, the rocks get larger. Today, much of this sedimentary rock can be seen in Utah s five national parks. 8 Fossils Dead plants and animals have, over time, become fossils. Fossils are formed when minerals interchange with the organic matter of a living thing that has died. Utah s oldest animal fossils are trilobites. 9 Dinosaurs The different rock layers of the Morrison Formation, where many of Utah s dinosaur bones have been uncovered, reflect what the region was like at the time. The world s most complete dinosaur skeletons have been found in the Morrison Formation. Nearly 23 complete dinosaurs and 300 partial dinosaurs have been found in quarries, or digs. You can see some of these digs at Dinosaur National Monument near Vernal, at the Cleveland-Lloyd Dinosaur Quarry in Emery County, in the Moab area, and in other places. Utah s state fossil = Allosaurus
4 10 Allosaurus Utahraptor
5 Assignment! Work Alone! Put your name on your paper Turn to page 29 in your textbooks. Read the passage that is entitled Douglas Discovers Dinosaurs in gray and answer the question below on your own sheet of paper: 1. Who is the story about? 2. For whom did he work? 3. What year did he begin to work for them? 4. What part of his work was very difficult? 5. How long did it take to extract the complete brontosaurus? 6. Where was this dinosaur originally displayed? 7. What is another name for this dinosaur? 8. To what places were many of Utah s dinosaur bones taken to (name three)? Carnivores vs. Herbivores Who know what the difference between carnivores and herbivores? In what category do you belong? Most likely you are neither. As humans, we eat both plants and animals. This is called an omnivore. What different plants and animals do you eat? What types of products are made from animals? From plants? Mountains Were Formed Many different movements of the Earth create mountains. Colliding of the Earths plates Sliding of the Earths plates Volcanic activity Erosion Fault lines are weak areas of the Earth s crust that more typically cause changes in the Earth s surface Is living on a fault line dangerous? Did you know that we all live on the Wasatch Fault? WSU, UofU, and BYU are all on the Wasatch Fault, and USU is close to another fault line
6 Wasatch Fault Line UofU says we have over EQ 700 per year Richter Scale 10x stronger per point 1-3 can t feel 4 or bigger you can feel Utah worries about an EQ of a 7 State Capitol
7 Volcanoes Made a Different Kind of Rock Igneous Rock lava rock. Molten or melted rock surfaces and hardens into what we know as lava, or igneous rock. Volcanoes the mountains from which lava comes out. All Utah volcanoes are extinct, or dead. Hot Springs Hot springs are formed when water comes in contact with hot rocks in the Earth s crust. Utah has many hot springs The Crater Heber City, Utah The Seabase Bonneville, Utah Natural Resources A natural resource is a material source of wealth that occurs in a natural state and has economic value Examples of some of Utah s natural resources Water Minerals Fossil fuels Wildlife animals Beautiful scenery Open space Dinosaur bones Forests & Timber Can you list more?
8 How do natural resources help Utah s economy? Farmers Miners Tourism Trade High Tech Industry Renewable Energy Available to Utah Renewable Geothermal (Heat stored in the earth) Biomass (Any living organism that can be burned & used as fuel) Derived from five distinct energy sources: Wood Garbage Landfill gases Alcohol Fuels Waste Water Wind Solar Non-Renewable Fossil Fuels (Fossil fuels are formed by the bodies of many plants and animals with a combination of heat and pressure over millions of years) Oil Natural Gas Coal Uranium Ore (Nuclear) Utah s Rock and Mineral Resources A Natural Resource is a material source of wealth, such as timber, fresh water, or a mineral deposit, that occurs in a natural state and has economic value. Utah is rich in fossil fuels: Coal, oil, and natural gas Coal used for power plants Utah also has a rich store of metals and minerals. Copper, gold, silver, and molybdenum Metals are often deposited through volcanic activity. Utah has enough salt to satisfy the worlds needs for 1,000 years. Other minerals are provided by the Great Salt Lake as well. Most of Utah s salt is used for snowy roads & water softeners. Large beds of sandstone, limestone, and quartz have been utilized here in Utah. A type of pure marble can also be found near Fillmore.
9 25 26 The Kennecott Utah Copper Mine Highest producing copper mine in the world The Most Recent Ice Age The last Ice Age helped to create the Utah we know today. About 10,000-12,000 years ago Glaciers were formed in the tops of the Utah mountains, some of which the remnants still remain (glacial lakes, small glaciers, etc.). Lake Bonneville was a huge lake created toward the end of the Ice Age. The Great Salt Lake, Utah Lake, and Sevier Lake were all in the area where Lake Bonneville stood. 27 Lake Bonneville Named by G. K. Gilbert in honor of Captain Benjamin Bonneville who explored a lot of the Western U. S.
10 28 Great Salt Lake Harvest millions of pounds of Brine Shrimp a year Bird and Fish food Robert Smithson s 1970 Spiral Jetty Assignment! Work alone! Ancient Lake Bonneville Turn to page 35 in your textbooks. Read all of the information on that page. Answer the following questions: 1. How many square miles was Lake Bonneville? 2. Compared to the Great Salt Lake, how deep did Lake Bonneville get? 3. Where did Lake Bonneville s water come from? 4. What are the three major remnants of Lake Bonneville? 5. What eventually happened to Lake Bonneville s water besides its losses from evaporation? 6. Can we see where Lake Bonneville s water levels used to be today? Ice Age Animals Many animal skeletons have been found in Utah and other parts of the U.S. that roamed the land during the Ice Age Deer, mammoths, giant sloths, ancient bison, musk ox, bears, and camels. Some animals have been found with spear points in them. What does this say about the Ice Age?
11 31 32 Natural Forces Are Still Shaping the Land Today 33 Erosion Wind Water Ice Heat Cold Other Changes Mud slides Rock slides Floods Earthquakes Quiz (20 points) 1. What do geologists study? (1 point) 2. What kind of rock covers much of Utah? (1 point) 3. What is Utah s oldest animal fossil? (1 point) 4. How were the Rocky Mountains formed (name two ways)? (2 point) 5. Earthquakes usually occur along what natural lines? (1 point) 6. Where does igneous rock come from? (1point) 7. Most of Utah s electricity is made from burning what? (1 point) 8. Why is the Great Salt Lake so salty? (3 points) 9. Which of today s lakes are believed to be remnants of the ancient Lake Bonneville? (3 points) 10. Name three Ice Age mammals. (3 points) 11. Name one way natural forces have changed the land during the last 50 years? (1 point) 12. What is Utah s state fossil? (1 point) 13. Utah has one of the biggest mines in the world. What is the name of this mine? (1 point)
Chapter 9: Earth s Past
Chapter 9: Earth s Past Vocabulary 1. Geologic column 2. Era 3. Period 4. Epoch 5. Evolution 6. Precambrian time 7. Paleozoic era 8. Shield 9. Stromatolite 10. Invertebrate 11. Trilobite 12. Index fossil
More informationRocks and Minerals What is right under your feet?
Rocks and Minerals What is right under your feet? Name: 1 Before you start What do you already know? What is the difference between a rock and a mineral? What are the three categories of rocks? 1. 2. 3.
More informationGeologic Time Scale Newcomer Academy Visualization Three
Geologic Time Newcomer Academy Visualization Three Chapter Subtopic/Media Key Points of Discussion Notes/Vocabulary Introduction Title NA NA Various Pictures of Geologic Time It s About Time Personal Timeline
More informationThe Fossil Record and Geologic Time Scale
Two Conceptions of Earth History: Catastrophism Assumption: Great Effects Require Great Causes Earth History Dominated by Violent Events Uniformitarianism Assumption: We Can Use Cause And Effect to Determine
More informationUnit 2 Lesson 4 The Geologic Time Scale. Copyright Houghton Mifflin Harcourt Publishing Company
Once Upon a Time How have geologists described the rate of geologic change? Geology is the scientific study of the origin, history, and structure of Earth and the processes that shape it. Early geologists
More information1. Michigan Geological History Presentation (Michigan Natural Resources)
1. Michigan Geological History Presentation (Michigan Natural Resources) The Michigan Geological History Presentation provides an overview of the approximately 3 billion years of Earth Processes that the
More informationThe rock cycle. Introduction. What are rocks?
The rock cycle This Revision looks at the three types of rock: sedimentary, igneous and metamorphic. It looks at how they are formed, the weathering of rocks and the way one form of rock turns into another,
More informationGeologic History Review
1. The climate that existed in an area during the early Paleozoic Era can best be determined by studying (1) the present climate of the area (2) recorded climate data of the area since 1700 (3) present
More informationEarth Science Landforms, Weathering, and Erosion Reading Comprehension. Landforms, Weathering, and Erosion
Reading Comprehension Name 1 How many people have been to the Rocky Mountains or the Grand Canyon? When people go to visit these natural wonders, they may not realize that it took millions of years for
More informationGeologic Time Scale Notes
Name: Date: Period: 1 2 3 4 5 6 7 Notes Essential Question: What is the geologic time scale? Vocabulary: Geology: the scientific study of the origin, history, and structure of Earth and the processes that
More informationChesapeake Bay Governor School for Marine and Environmental Science
Choose the best answer and write on the answer sheet provided. 1. Which of the following is LEAST likely to be an effect of global warming? (a) Loss of fertile delta regions for agriculture (b) Change
More informationCarbonate Rock Formation
Limestone, dolomite (or dolostone), and marble are often collectively referred to as carbonate rocks because the main mineral is calcite. The chemical name of calcite is calcium carbonate. Limestone, dolomite,
More informationRocks & Minerals. 10. Which rock type is most likely to be monomineralic? 1) rock salt 3) basalt 2) rhyolite 4) conglomerate
1. Of the Earth's more than 2,000 identified minerals, only a small number are commonly found in rocks. This fact indicates that most 1) minerals weather before they can be identified 2) minerals have
More informationWhat are Rocks??? Rocks are the most common material on Earth. They are a naturally occurring collection of one or more minerals.
The Rock Cycle What are Rocks??? Rocks are the most common material on Earth. They are a naturally occurring collection of one or more minerals. The Rock Cycle a cycle that continuously forms and changes
More informationWhat is a rock? How are rocks classified? What does the texture of a rock reveal about how it was formed?
CHAPTER 4 1 The Rock Cycle SECTION Rocks: Mineral Mixtures BEFORE YOU READ After you read this section, you should be able to answer these questions: What is a rock? How are rocks classified? What does
More informationUnit 5: Formation of the Earth
Unit 5: Formation of the Earth Objectives: E5.3B - Explain the process of radioactive decay and explain how radioactive elements are used to date the rocks that contain them. E5.3C - Relate major events
More informationCh6&7 Test. Multiple Choice Identify the choice that best completes the statement or answers the question.
Ch6&7 Test Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Which of the following does NOT change the form of existing rock? a. tremendous pressure c.
More information3 The Mesozoic and Cenozoic Eras
CHAPTER 9 3 The Mesozoic and Cenozoic Eras SECTION A View of Earth s Past KEY IDEAS As you read this section, keep these questions in mind: What were the periods of the Mesozoic and Cenozoic Eras? What
More informationName: LAB: The Geologic Time Scale
Name: LAB: The Geologic Time Scale INTRODUCTION: It is difficult to comprehend the age of the Earth and the time that various geologic events occurred in the past. A model drawn to scale is often useful
More informationIgneous rocks formed when hot molten material (magma) cools and hardens (crystallizes).
Objectives You will learn about how the land of North Dakota was formed. Introduction North Dakota is a wonderful place to live. Have you ever though about how it was formed? To answer that question, you
More informationUnderstanding Geologic Time from the Texas Memorial Museum
Understanding Geologic Time from the Texas Memorial Museum Objective To gain a better understanding of the geologic time scale. Materials Activity 1: Geologic Time Geologic Time Activity Worksheet (included)
More informationSedimentary Rock Formation Models. 5.7 A Explore the processes that led to the formation of sedimentary rock and fossil fuels.
Sedimentary Rock Formation Models 5.7 A Explore the processes that led to the formation of sedimentary rock and fossil fuels. The Formation Process Explained Formation of these rocks is one of the important
More informationFIRST GRADE ROCKS 2 WEEKS LESSON PLANS AND ACTIVITIES
FIRST GRADE ROCKS 2 WEEKS LESSON PLANS AND ACTIVITIES ROCK CYCLE OVERVIEW OF FIRST GRADE CHEMISTRY WEEK 1. PRE: Comparing solids, gases, liquids, and plasma. LAB: Exploring how states of matter can change.
More informationDo-Now. 1.) Get out notebook.
Do-Now 1.) Get out notebook. 2.) Answer the following questions on the first clean sheet in your notebook. 1.) What are renewable resources? 2.) What are nonrenewable resources? Alternative Sources of
More informationHow can you tell rocks apart?
How can you tell rocks apart? Grade Range: 4-7 G.L.E Focus: 1.1.5 Time Budget: 1 1.5 hours WASL Vocabulary: Overview: Different rocks have different characteristics because of their minerals, the ways
More informationRapid Changes in Earth s Surface
TEKS investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes, and landslides Rapid Changes in Earth s Surface Constant Changes Earth s surface is constantly changing. Wind,
More information89.215 - FORENSIC GEOLOGY GEOLOGIC TIME AND GEOLOGIC MAPS
NAME 89.215 - FORENSIC GEOLOGY GEOLOGIC TIME AND GEOLOGIC MAPS I. Introduction There are two types of geologic time, relative and absolute. In the case of relative time geologic events are arranged in
More informationFROM SEDIMENT INTO SEDIMENTARY ROCK. Objectives. Sediments and Sedimentation
FROM SEDIMENT INTO SEDIMENTARY ROCK Objectives Identify three types of sediments. Explain where and how chemical and biogenic sediments form. Explain three processes that lead to the lithification of sediments.
More informationAnswer Keys to Unit Tests
Reading Geography Series Answer Keys to Unit Tests Unit 1 The Five Themes of Geography Unit 2 Patterns in Physical Geography Unit 3 Natural Resources 7 Portage & Main Press Unit Test for The Five Themes
More informationGeologic Time. Relative Dating. Principle of Original Horizontality. Relative Time. Absolute Time. Geologic Column
Geologic Time Relative Time 5 Principles of Relative Dating Absolute Time Radiometric Dating Geologic Column Relative Dating principle of horizontality principle of superposition principle of cross-cutting
More informationSedimentary Rocks. Find and take out 11B-15B and #1 From Egg Carton
Sedimentary Rocks Find and take out 11B-15B and #1 From Egg Carton Erosion Erosion is a natural process where rocks and soil are Broken and Moved We will focus on 4 types of erosion; Wind, Rain, Ice and
More informationFourth Grade Geology: The Earth and Its Changes Assessment
Fourth Grade Geology: The Earth and Its Changes Assessment 1a. What is the center layer of the Earth called? a. crust b. core c. mantle d. middle 1b. Label each layer of the Earth. 1c. What are the Earth
More informationOcean Floor Continental Slope Begins at the Continental Shelf Very sharp drop to depths over 2 miles Covered with thick layers of sand, mud, and rocks
Ocean Floor Continental Shelf Begins at the shoreline Gently slopes underwater Average depth of 430 feet Thick layers of sand, mud, and rocks The beach is part of the Continental Shelf Ocean Floor Continental
More information6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes
Name: Date: 1. The road shown below was suddenly broken by a natural event. 3. The convergence of two continental plates would produce Which natural event most likely caused the crack in the road? island
More informationRocks and Plate Tectonics
Name: Class: _ Date: _ Rocks and Plate Tectonics Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What is a naturally occurring, solid mass of mineral or
More informationGEOL 104 Dinosaurs: A Natural History Geology Assignment. DUE: Mon. Sept. 18
GEOL 104 Dinosaurs: A Natural History Geology Assignment DUE: Mon. Sept. 18 Part I: Environments of Deposition Geologists can use various clues in sedimentary rocks to interpret their environment of deposition:
More informationTECTONICS ASSESSMENT
Tectonics Assessment / 1 TECTONICS ASSESSMENT 1. Movement along plate boundaries produces A. tides. B. fronts. C. hurricanes. D. earthquakes. 2. Which of the following is TRUE about the movement of continents?
More informationNATURAL REGIONS OF KENTUCKY
NATURAL WONDERS As you travel around Kentucky taking pictures, you are excited by what you see. Kentucky offers diverse and amazing sights. The Six Regions In the West, you see the Mississippi River, the
More informationWorksheet A Environmental Problems
Worksheet A Environmental Problems Vocabulary Can you talk about Environmental issues in English? With a partner, try to explain the terms in the diagram below. Why are the words divided into two groups
More informationGrade 9 Geography - Unit 3 Lesson 3 The Rock Cycle
Grade 9 Geography - Unit 3 Lesson 3 The Rock Cycle What is the difference between a Rock and a Mineral? Minerals are homogeneous, naturally occurring, inorganic solids. Each mineral has a definite chemical
More informationThe Next Generation Science Standards (NGSS) Correlation to. EarthComm, Second Edition. Project-Based Space and Earth System Science
The Next Generation Science Standards (NGSS) Achieve, Inc. on behalf of the twenty-six states and partners that collaborated on the NGSS Copyright 2013 Achieve, Inc. All rights reserved. Correlation to,
More informationGEL 113 Historical Geology
GEL 113 Historical Geology COURSE DESCRIPTION: Prerequisites: GEL 111 Corequisites: None This course covers the geological history of the earth and its life forms. Emphasis is placed on the study of rock
More informationThe Earth, Sun, and Moon
reflect The Sun and Moon are Earth s constant companions. We bask in the Sun s heat and light. It provides Earth s energy, and life could not exist without it. We rely on the Moon to light dark nights.
More information4. Plate Tectonics II (p. 46-67)
4. Plate Tectonics II (p. 46-67) Seafloor Spreading In the early 1960s, samples of basaltic ocean crust were dredged up from various locations across the ocean basins. The samples were then analyzed to
More informationThe Earth System. The geosphere is the solid Earth that includes the continental and oceanic crust as well as the various layers of Earth s interior.
The Earth System The atmosphere is the gaseous envelope that surrounds Earth. It consists of a mixture of gases composed primarily of nitrogen, oxygen, carbon dioxide, and water vapor. The atmosphere and
More informationGreater Nanticoke Area School District Science/Technology Standards 5 th Grade
Greater Nanticoke Area School District Science/Technology Standards 5 th Grade Standard 3.1 Unifying Themes CS 3.1.7A Explain the parts of a simple system and their relationship to each other 1. Describe
More informationName Class Date WHAT I KNOW. about how organisms have changed. grown in complexity over time.
History of Life Evolution Q: How do fossils help biologists understand the history of life on Earth? 19.1 How do scientists use fossils to study Earth s history? WHAT I KNOW SAMPLE ANSWER: Fossils give
More informationROCKS OF THE GRAND CANYON BACKGROUND INFORMATION FOR DOCENTS
ROCKS OF THE GRAND CANYON BACKGROUND INFORMATION FOR DOCENTS There are three distinct types of rock. Igneous rocks. Igneous comes from the Greek word for fire. It is so hot deep in the Earth that rocks
More informationSection 1 Earth s surface undergoes gradual and sudden changes
Section 1 Earth s surface undergoes gradual and sudden changes Student Class 1. Scientists estimate the age of the Earth to be about 4.6 billion years old, using evidence and theories. Then they construct
More informationUnit 4: The Rock Cycle
Unit 4: The Rock Cycle Objective: E 3.1A Discriminate between igneous, metamorphic, and sedimentary rocks and describe the processes that change one kind of rock into another. E 3.1B Explain the relationship
More informationGeologic Time. This page last updated on 08-Oct-2015
Page 1 of 16 EENS 1110 Tulane University Physical Geology Prof. Stephen A. Nelson Geologic Time This page last updated on 08-Oct-2015 From the beginning of this course, we have stated that the Earth is
More informationHow Did These Ocean Features and Continental Margins Form?
298 10.14 INVESTIGATION How Did These Ocean Features and Continental Margins Form? The terrain below contains various features on the seafloor, as well as parts of three continents. Some general observations
More informationFoundations of Earth Science (Lutgens and Tarbuck, 6 th edition, 2011)
EAS 100 Study Guide to Textbook Foundations of Earth Science (Lutgens and Tarbuck, 6 th edition, 2011) STUDY GUIDE 8/2010 The textbook for EAS 100, Foundations of Earth Science, by Lutgens and Tarbuck
More informationContinents join together and split apart.
KEY CONCEPT Continents change position over time. BEFORE, you learned Earth s main layers are the core, the mantle, and the crust The lithosphere and asthenosphere are the topmost layers of Earth The lithosphere
More informationEvolution (18%) 11 Items Sample Test Prep Questions
Evolution (18%) 11 Items Sample Test Prep Questions Grade 7 (Evolution) 3.a Students know both genetic variation and environmental factors are causes of evolution and diversity of organisms. (pg. 109 Science
More informationRide the Rock Cycle. Suggested Goals: Students will gain an understanding of how a rock can move through the different stages of the rock cycle.
Illinois State Museum Geology Online http://geologyonline.museum.state.il.us Ride the Rock Cycle Grade Level: 5 6 Purpose: To teach students that the rock cycle, like the water cycle, has various stages
More informationAlternative Energy. Terms and Concepts: Relative quantities of potential energy resources, Solar constant, Economies of scale
Objectives Key Terms and Concepts Introduction Solar Wind Hydroelectric Power Geothermal Sources Biofuels Summary: Economies of Scale Questions for the video if time permits Alternative Energy Objectives:
More informationRENEWABLE OR NOT? ADVANCE PREPARATION MATERIALS
AT A GLANCE RENEWABLE OR NOT? Students learn the difference between renewable and non-renewable resources and discover why sustainable use of natural resources is important. OBJECTIVES Students will: Identify
More informationExploring How Rocks Are Formed
Exploring How Rocks Are Formed Grade Level: 3-4 Purpose and Goals: In this lesson, students are introduced to the three types of rocks: igneous, sedimentary, and metamorphic. After receiving background
More informationModified Richter Scale
Name Date ID Grade 7 - Science Interim Assessment Third Grading Period 1. Which of the following is NOT affected by the tilt of Earth's axis? Length of day Type of climate Change of seasons Length of year
More information5 th Grade Science Vocabulary Words
5 th Grade Science Vocabulary Words abiotic factor A nonliving part of an ecosystem. acceleration Change in velocity with respect to time. action The force one object applies to a second, as in Newton
More informationThe Ice Age By: Sue Peterson
www.k5learning.com Objective sight words (pulses, intermittent, isotopes, chronicle, methane, tectonic plates, volcanism, configurations, land-locked, erratic); concepts (geological evidence and specific
More information1. The diagram below shows a cross section of sedimentary rock layers.
1. The diagram below shows a cross section of sedimentary rock layers. Which statement about the deposition of the sediments best explains why these layers have the curved shape shown? 1) Sediments were
More informationChapter 8: Plate Tectonics -- Multi-format Test
Name: Class: Date: ID: A Chapter 8: Plate Tectonics -- Multi-format Test Modified True/False Indicate whether the statement is true or false. If false, change the identified word or phrase to make the
More informationThe Polar Climate Zones
The Polar Climate Zones How cold is it in the polar climate? Polar areas are the coldest of all the major climate zones The Sun is hardly ever high enough in the sky to cause the plentiful ice to melt,
More informationROCKS, FOSSILS AND SOILS SECTION 8: FOSSILS From Hands on Science by Linda Poore, 2003
ROCKS, FOSSILS AND SOILS SECTION 8: FOSSILS From Hands on Science by Linda Poore, 2003 STANDARDS: Westminster College Students will write or draw descriptions of a sequence of steps, events and observations,
More informationWeathering, Erosion, and Soils. Weathering and Erosion. Weathering and Erosion
Weathering, Erosion, and Soils 1 The Grand Canyon, a landscape shaped by weathering and erosion 2 Weathering vs. erosion Types of weathering Physical Chemical Rates of weathering and erosion Climate Rock
More informationWhat s It All About? The Sun as a Power Source Instructor Guide
What s It All About? The Sun as a Power Source Instructor Guide Subject Area Unit Grade Time Science Earth Science K - 1st grade 45 minutes Overview This activity reinforces the concept that the sun supplies
More informationThe Formation of Fossil Fuels
The Formation of Fossil Fuels There are many sources of energy in our world. We can get energy from the sun, from wind, and from falling water. We can also get energy from materials that contain stored
More information5-Minute Refresher: RENEWABLE ENERGY
5-Minute Refresher: RENEWABLE ENERGY Renewable Energy Key Ideas Renewable energy is a source of energy that can be used and replenished naturally in a relatively short period of time. Non renewable energy
More informationHistory of the Earth/Geologic Time 5E Unit
History of the Earth/Geologic Time 5E Unit Description: Students will create a timeline of Earth history in the classroom and learn about major changes to the Earth and life through time. Standards Targeted:
More informationFORMATION OF EARTH. Today we are going to talk about the earth.how it was formed.
FORMATION OF EARTH Have you ever wondered about the universe? What made it possible.how it was formed? Of course, religion has explained for centuries the intricacies of creation. And as always, science
More informationClimate, Vegetation, and Landforms
Climate, Vegetation, and Landforms Definitions Climate is the average weather of a place over many years Geographers discuss five broad types of climates Moderate, dry, tropical, continental, polar Vegetation:
More informationNorth America North American Diversity
Non-fiction: North America North American Diversity North America North American Diversity North America is diverse in many ways. Every type of ecosystem 1 that exists on Earth exists somewhere in North
More informationConventional Energy Sources
9.2 Conventional Energy Sources Key Question: What benefits and problems come with common sources of energy? Hints The word plant here is not the kind that grows out of the ground. In this section, plants
More informationPlate Tectonics. Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics. And I am Buddy Zed s mascot
Plate Tectonics Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics And I am Buddy Zed s mascot Continental Drift Alfred Wegener proposed that continents were not always where
More informationPlate Tectonics Short Study Guide
Name: Class: Date: Plate Tectonics Short Study Guide Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The existence of coal beds in Antarctica
More informationAlfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics. Wegener in Greenland about 1912. He froze to death there in 1930.
Alfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics Wegener in Greenland about 1912. He froze to death there in 1930. Science is self correcting. The Scientific Method The history
More informationMixtures. reflect. How is seawater different from pure water? How is it different from rocky soil?
reflect Everything around us is made out of tiny bits of matter. These particles may combine in different ways to produce new materials. Sometimes we need to separate the parts of a material. If we know
More information[Geology Layers of the Earth] [Basic: Grade 2-3] [Advanced: Grade 5: Introduction to Plate Tectonics}
[Geology Layers of the Earth] [Basic: Grade 2-3] [Advanced: Grade 5: Introduction to Plate Tectonics} BACKGROUND Scientists and geologists have been able to do some drilling on Earth. They are also able
More informationFoundations of Earth Science (Lutgens and Tarbuck, 5 th edition, 2008)
EAS 100 Study Guide to Textbook Foundations of Earth Science (Lutgens and Tarbuck, 5 th edition, 2008) STUDY GUIDE 1/08 The textbook for EAS 100, Foundations of Earth Science, by Lutgens and Tarbuck is
More informationGETTING TO THE CORE: THE LINK BETWEEN TEMPERATURE AND CARBON DIOXIDE
DESCRIPTION This lesson plan gives students first-hand experience in analyzing the link between atmospheric temperatures and carbon dioxide ( ) s by looking at ice core data spanning hundreds of thousands
More informationAll sediments have a source or provenance, a place or number of places of origin where they were produced.
Sedimentary Rocks, Processes, and Environments Sediments are loose grains and chemical residues of earth materials, which include things such as rock fragments, mineral grains, part of plants or animals,
More informationSantillana Intensive English Levels 4-6
Santillana Intensive English Levels 4-6 California Science Content Standards Grades 4-6 Grade 4 Physical Sciences 1. Electricity and magnetism are related effects that have many useful applications in
More informationBASIC LESSON Objective(s)
[Geology - Landforms] [K-1: Basic] [Grades 2-3: Advanced] BACKGROUND Landforms are natural features of the Earth's surface. They are created by the movement of ice or water, earthquakes, lava flows, volcanoes,
More informationWEATHERING, EROSION, AND DEPOSITION PRACTICE TEST. Which graph best shows the relative stream velocities across the stream from A to B?
NAME DATE WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST 1. The diagram below shows a meandering stream. Measurements of stream velocity were taken along straight line AB. Which graph best shows the
More informationEssential Standards: Grade 4 Science Unpacked Content
This document is designed to help North Carolina educators teach the Essential Standards (Standard Course of Study). NCDPI staff are continually updating and improving these tools to better serve teachers.
More informationUnit 4 Lesson 2 Plate Tectonics. Copyright Houghton Mifflin Harcourt Publishing Company
Puzzling Evidence What evidence suggests that continents move? In the late 1800s, Alfred Wegener proposed his hypothesis of continental drift. According to this hypothesis, the continents once formed a
More informationA: Planets. Q: Which of the following objects would NOT be described as a small body: asteroids, meteoroids, comets, planets?
Q: Which of the following objects would NOT be described as a small body: asteroids, meteoroids, comets, planets? A: Planets Q: What can we learn by studying small bodies of the solar system? A: We can
More informationES Chapter 10 Review. Name: Class: Date: Multiple Choice Identify the choice that best completes the statement or answers the question.
Name: Class: Date: ES Chapter 10 Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Scientists used the pattern of alternating normal and reversed
More informationThird Grade Science Vocabulary Investigation Design & Safety
recycle dispose reuse goggles data conclusion predict describe observe record identify investigate evidence analyze mass matter float sink attract force magnet magnetic magnetism pole pull push repel Third
More informationLesson Title: Kincaid Creatures Subject: Texas history, science, math By: Carol Schlenk. Grade level: 7 th (Can be modified for 4 th grade)
Lesson Title: Kincaid Creatures Subject: Texas history, science, math By: Carol Schlenk Grade level: 7 th (Can be modified for 4 th grade) Rationale or Purpose: To illustrate how archeologists use stratigraphy
More informationA ROCK. naturalists. Young. Would you like to hear a good story? Ask a rock.
Young naturalists ASK A ROCK Would you like to hear a good story? Ask a rock. Big or small, sharp or round, each rock you see has a tale to tell about how the land around it has been shaped for millions
More informationLesson Plan Title. Toilet Paper Tape Measure of Geologic Time
Lesson Plan Title Toilet Paper Tape Measure of Geologic Time Name (last, first): Serratos, Danielle J. Scientific Theme(s): Life Science *Changes in Life Forms over Time Earth Science *Forces that Shape
More informationScope and Sequence Interactive Science grades 6-8
Science and Technology Chapter 1. What Is Science? 1. Science and the Natural World 2.Thinking Like a Scientist 3. Scientific Inquiry Scope and Sequence Interactive Science grades 6-8 Chapter 2. Science,
More informationGeorgia Performance Standards Framework for Science Grade 6. Unit Organizer: Geology: Inside the Earth (Approximate Time: 7 Weeks)
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
More informationCHEMICAL SIGNATURES OF ASTEROID IMPACTS
CHEMICAL SIGNATURES OF ASTEROID IMPACTS INTRODUCTION The film The Day the Mesozoic Died identifies the presence of high quantities of iridium (Ir) in the clay layer at the boundary between the Cretaceous
More informationCharacteristics of Sedimentary Rocks
Characteristics of Sedimentary Rocks Deposited at the earth s surface by wind, water, glacier ice, or biochemical processes Typically deposited in strata (layers) under cool surface conditions. This is
More informationClimate Change: A Local Focus on a Global Issue Newfoundland and Labrador Curriculum Links 2010-2011
Climate Change: A Local Focus on a Global Issue Newfoundland and Labrador Curriculum Links 2010-2011 HEALTH Kindergarten: Grade 1: Grade 2: Know that litter can spoil the environment. Grade 3: Grade 4:
More informationFOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FOURTH GRADE VOLCANOES WEEK 1. PRE: Comparing different structures of volcanoes. LAB: Modeling three types
More information