November 3, SWABT interpret cross-sections with index fossils and unconformities to determine relative ages of rock layers.
|
|
- Laureen Ray
- 5 years ago
- Views:
Transcription
1 Aims: November 3, 2016 SWABT interpret cross-sections with index fossils and unconformities to determine relative ages of rock layers. Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: Homework: EH.5 Unconformities How will you help our class earn all of our S.T.R.I.V.E. Points? UNIT TEST COUNTDOWN: 4 study days! 1
2 Aim Check: 2
3 SCIENCE 8 Unconformities EH.5 Name: Date: Homeroom: Earth s History Shoooo I m GROWN! OBJECTIVES: By the end of class, students will be able to SWABT interpret cross-sections with index fossils and unconformities to determine relative ages of rock layers. DO NOW 1. The picture shows a rock formation with folded layers. Which statement best explains how the rock layers folded? A. The rock melted and flowed downhill. B. The rock was deformed by a meteorite impact. C. The rock was suddenly pulled apart during an earthquake. D. The rock was slowly compressed due to tectonic plate movement. 2. What would this collision do to the strata? How could this affect the Law of Superposition? The cross section below shows the movement of wind-driven sand particles that strike a partly exposed basalt cobble located at the surface of a windy desert. 3. What would this process do to the strata? How could this affect the Law of Superposition? 3
4 CLASS NOTES DRAKE <3 s GEOLOGY... LAW OF SUPERPOSITION INDEX FOSSILS Fossils can tell the relative age of the rock layer and o o Easy peasy, but what about when the layers look like this? 4
5 HUTTON still kinda a big deal While developing his idea of Hutton became very interested in the rock outcrop shown below. He soon realized that according to uniformitarianism, the lower rocks must have been: Therefore, there must be some period of time that is NOT represented between the formations of these two units! UNCONFORMITY: 5
6 DISRUPTIONS EXTRUSION : Younger than rock below it INTRUSION: FAULT: younger than layers it goes through What layer is the youngest? 6
7 Guided Practice Following is a description of the geologic history of a region. A large sea covered the region, allowing coral reefs to develop. Next, the sea retreated and the region became desert. Then, geological stresses caused surface rocks to crack and break. Finally, the deep cracks in the surface rocks allowed lava to erupt and extrude, which then quickly cooled. The layers M, N, and O represent the position of three rock layers found in the region. The layers have not been overturned. Select the boxes to match the geologic features or materials that will likely be found in the layers, based on the region s geologic history Layer M Layer N Layer O Fault Basalt (igneous) Limestone (sedimentary) Sandstone (sedimentary) 7
8 Directions: Answer the following questions in COMPLETE sentences. ICE to support your answer 3. Use the cross section to explain how the geologist knows that the flow labeled on the picture is older than the shale. 4. Use the cross section to explain how the geologist knows the relative age of the intrusion compared with that of the gravel. 8
9 Independent Practice Directions: For each key term, explain the big idea to a kindergartener. Then, draw a picture to illustrate the word. Term Concept Picture UNCONFORMITY INTRUSION EXTRUSION FAULT 9
10 Use the picture below to answer questions Order the layers from oldest to youngest. 2. Explain what an intrusion is and how old it is relative to the layers of rock around it. 3. How could a scientist use the fossil in layer B to date a rock layer in another location? Examine the following diagrams. Order the layers of rock from oldest to youngest. Remember it is easiest to do this by starting with the oldest (bottom) and working up to the youngest. The diagrams start simple and get beastier and beasier! 10
11 What rock is layer B made of? What type of rock is layer B? How is that rock formed? 11
12 What type of disruption is layer F most likely to be? How is that rock formed? 12
13 You Do: REVIEW! (comps are coming up faaaaast ) 1. According to the theory of uniformitarianism, A. geologic processes we observe today have operated in the past B. geologic process in the past operated at the same rate as they do today C. all of the planets formed from a uniform solar nebula D. early Earth was covered by a uniform magma ocean 2. James Hutton ( ) is often referred to as the father of modern geology. His detailed observations and theories about Earth processes opposed the accepted theories of his time. One of his contributions was the development of what he called the great geological cycle. Hutton theorized that most rocks were igneous in origin. The igneous rocks could then change into sedimentary or metamorphic rocks. The chart below shows locations of several rock types and the minerals they contain. What evidence from the chart could be used to support Hutton s theory that most rocks are igneous in origin? A. Igneous rocks are only found in Germany. B. Sedimentary rocks are found in both North America and England. C. The rocks found in the table are made up of many of the same minerals. D. The rocks found in the table are different types of rocks from different locations. 3. Which of these statements about the modern version of uniformitarianism is correct? A. Rapid change is solely responsible for Earth's features. B. Geologists no longer believe any of the concept to be true. C. It completely ignores the role of catastrophic events in shaping Earth's features. D. It includes the role of occasional, catastrophic events in shaping Earth's features. 13
14 4. Which of the following pieces of evidence would be most helpful to a historian studying the amount of rainfall at Plymouth Colony in 1620? A. a fossil B. a tree ring C. ripple marks in a rock D. an ice core 5. Catastrophism assumes that the Earth s surface was shaped by violent, short-lived natural events. Describe an example that a geologist would define as a catastrophic event. Then, explain how this event can be used to support the Theory of Uniformitarianism. 6. An unusual type of fossil clam is found in rock layers high in the Swiss Alps. The same type of fossil clam is also found in the Rocky Mountains of North America. From this, scientists conclude that A. glaciers carried the fossils up the mountains B. the Rocky Mountains and the Swiss Alps are both volcanic in origin C. clams once lived in mountains, but have since evolved into sea-dwelling creatures D. the layers of rocks in which the fossils were found are from the same geologic age 14
15 Science 8 Name: SKILL SNAPSHOT Date: EH.5: Unconformities Homeroom: Quick Notes: Read and ANNOTATE each question before you solve the problem. Like A Scholar? Yes No Redo? Yes No Directions: Support your selection by finding evidence to support your answer OR evidence to support why another is incorrect. Start your explanation with The evidence shows that Question 1. What geologic process accounts for the difference in the arrangement of the rock layers? Supporting evidence A. erosion B. intrusion C. faulting D. extrusion 2. The Law or Superposition says that A. The rock layers that are on top are less dense B. The rock layers that are on top are older C. The rock layers that are on the bottom are older D. The rock layers that are on the bottom are less dense 3. Mrs. Petrozzi claims that a fossil found is 200,000 years old according to generally accepted radioactive dating procedures. Mr. Parker disputes the accuracy of the age because the fossil was found closer to the Earth's surface than were previously discovered fossils of the same age. Which of the following should Mrs. Petrozzi use as evidence to support her finding? A. Fossils form only under certain conditions. B. Older rock layers may be pushed closer to the surface by geologic processes. C. Older rock layers commonly lie deeper underground than younger ones. D. The age of a rock layer can often help in determining the age of the fossils it contains. 15
16 4. The picture below shows a geologic cross-section of rock layers in a specific area. KEY W = intrusion X = silt layer Y = unconformity Z = sandstone layer Feature W represents an intrusion. Choose two other labeled features/layers in the geologic crosssection and identify their relative age with relation to intrusion W. Support each answer with specific information about the cross-cutting relationship from the crosssection. 5. The magnified views shown of the minerals found in an igneous rock and in a metamorphic rock. The millimeter scale indicates the size of the crystals shown in the views. Identify the environment of formation of the igneous rock based on the size of the crystals. Then, explain how grain size supports your conclusion. 16
November 1, Aims: Agenda. SWABT explain the absolute age of rocks using radiometric dating.
Aims: November 1, 2016 SWABT explain the absolute age of rocks using radiometric dating. Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: Homework: HE.3
More informationNovember 2, Aims: Agenda. SWABT explain the relative age of rocks using the Law of Superposition and index fossils.
Aims: November 2, 2016 SWABT explain the relative age of rocks using the Law of Superposition and index fossils. Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing
More informationState the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks.
Objectives State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks. Compare three types of unconformities. Apply the law of crosscutting
More informationGeology Test Review Answers
Name: Geology Test Review Answers Core: Fill in the blanks: 1. Sediments get compacted and cemented into sedimentary rock. 2. Igneous rocks can be intrusive or extrusive from a volcano. 3. Adding heat
More informationEarth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes.
Earth s History Date: Been There, Done That What is the principle of uniformitarianism? The principle of states that geologic processes that happened in the past can be explained by current geologic processes.
More informationDirected Reading page
Skills Worksheet Directed Reading page 185-190 Section: Determining Relative Age 1. How old is Earth estimated to be? 2. Who originated the idea that Earth is billions of years old? 3. On what did the
More informationOctober 5, Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: Homework: ES.9 Metamorphic Rocks
October 5, 2016 Aims: SWBAT describe the formation of metamorphic rocks. SWBAT use the composition of a metamorphic rock to identify the rock and to infer its history of formation. Agenda 1. Do Now 2.
More informationOctober 4, Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: Homework: ES.8 Sedimentary Rocks
October 4, 2016 Aims: SWBAT describe the formation of sedimentary rocks. SWBAT use the composition of a sedimentary rock to identify the rock and to infer its history of formation. Agenda 1. Do Now 2.
More information3. [ES 3] 1. [ST8.2] Some processes that shape Earth s surface are slow. Other processes are rapid. Which statement describes a rapid change?
Science 8 SCIENCE QUARTERLY ASSESSMENT 2 3. [ES 3] S 1. [ST8.2] Some processes that shape Earth s surface are slow. Other processes are rapid. Which statement describes a rapid change? A. Glaciers melt
More informationNotepack 18 AiM: How can we tell the age of rock layers? Do now: Which Jenga piece was placed first to build this tower? Support your answer with
Notepack 18 AiM: How can we tell the age of rock layers? Do now: Which Jenga piece was placed first to build this tower? Support your answer with complete sentences. How old is the Earth? The Earth is
More informationB) color B) Sediment must be compacted and cemented before it can change to sedimentary rock. D) igneous, metamorphic, and sedimentary rocks
1. Which characteristic of nonsedimentary rocks would provide the least evidence about the environment in which the rocks were formed? A) structure B) color C) crystal size D) mineral composition 2. Which
More informationL wave Lahar Lava Magma
Very large collapsed volcanic crater, often containing a lake eg. Lake Taupo The process which provides the force to move the tectonic plates Innermost part of the Earth, made of a liquid outer core and
More informationEarth Science Unit 1 Review
Name: Date: 1. The picture below shows a model of the rock cycle. 2. rock cycle diagram is shown below. During which part of the rock cycle does water break rocks apart?. part 1 B. part 2. part 3 D. part
More informationSeptember 14, SWBAT explain how divergent boundaries shape Earth s surface.
September 14, 2016 Aims: SWBAT explain how divergent boundaries shape Earth s surface. Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: Homework: EI.11
More informationCHAPTER 8 DETERMINING EARTH S AGE RELATIVE AND ABSOLUTE ROCK AGES. Loulousis
CHAPTER 8 DETERMINING EARTH S AGE RELATIVE AND ABSOLUTE ROCK AGES Loulousis Bellringer What are 5 visual clues that help you determine if someone is older or younger than you? Color of hair Wrinkles in
More informationTRACE FOSSIL FOSSIL ICE CORE RELATIVE DATING SUPERPOSITION ABSOLUTE DATING GEOLOGIC COLUMN UNIFORMITARIANISM HALF-LIFE RADIOACTIVE DECAY
THIS IS NOT THE SAME TEST. YOU MUST ANSWER ALL QUESTIONS. NAME: Bubble the circle below U3L1 Write the letter next to the vocab term VOCAB MATCH 1 A. O B. O C. O D. O 1 2 A. O B. O C. O D. O 2 3 A. O B.
More informationENVI.2030L Geologic Time
Name ENVI.2030L Geologic Time I. Introduction There are two types of geologic time, relative and absolute. In the case of relative time geologic events are arranged in their order of occurrence. No attempt
More informationDetermining Earth's History Rocks and Ice Cores
Earths History Reu2.notebook November 14, 2013 Determining Earth's History Rocks and Ice Cores One goal of geology is to develop a timeline of Earth's past, including both geological and biological events.
More informationThe Geology of Pacific Northwest Rocks & Minerals Activity 1: Geologic Time
Name: Age: I. Introduction There are two types of geologic time, relative and absolute. In the case of relative time geologic events are arranged in their order of occurrence. No attempt is made to determine
More informationRocks. Geology: Slides 22-50
Rocks Geology: Slides 22-50 Rocks Catastrophism versus Uniformitarianism Catastrophism The Earth s surface was created by fast drastic changes (called catastrophes) that occurred long ago and do not occur
More informationGeneral Geology Lab #7: Geologic Time & Relative Dating
General Geology 89.101 Name: General Geology Lab #7: Geologic Time & Relative Dating Purpose: To use relative dating techniques to interpret geological cross sections. Procedure: Today we will be interpreting
More informationStation Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus
Station 1 1. Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus 2. Look at the fossil labeled #7. Identify each of the following: a. Kingdom b. Phylum
More informationName Geo 4 Practice Match the principle on the left (column A) with the definition (or part of the definition) on the right (column B).
Name Geo 4 Practice 1 Target 1 2 3 4 Geo 4 I can define the create, alter and/or destroy the rock record. I can interpret a diagram to determine the sequence of events (relative age) in Earth s history
More informationRelative Dating. The Rock Cycle. Key Concept Scientists can interpret the sequence of events in Earth s history by studying rock layers.
2 What You Will Learn The rock cycle includes the formation and recycling of rock. Relative dating establishes the order in which rocks formed or events took place. The principle of superposition states
More informationb. atomic mass H What is the density of an object with a volume of 15cm 3 and a mass of 45g?
Name Period Date Earth Science Midterm Review 2015-2016 Quarter 1 Review Assign #1 Basic Chemistry An atom is a basic chemical building block of matter. An atom consists of protons, neutrons, and electrons.
More informationSeptember 2, Aims: Agenda. SWBAT explain Alfred Wegener s hypothesis of Continental Drift.
September 2, 2016 Aims: SWBAT explain Alfred Wegener s hypothesis of Continental Drift. Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: Homework: EI.6
More informationClassify Rock (rock1)
Name: Date: 1. Cleavage of a mineral is related to a mineral's A. chemical composition. B. streak color. C. luster. D. crystalline structure. 2. Which is not part of the definition of a mineral? A. naturally
More informationUnit 6: Interpreting Earth s History
Unit 6: Interpreting Earth s History How do we know that the Earth has changed over time? Regent s Earth Science Name: Topics Relative Dating Uniformitarianism Superposition Original Horizontality Igneous
More informationSection 1: Earth s Interior and Plate Tectonics Section 2: Earthquakes and Volcanoes Section 3: Minerals and Rocks Section 4: Weathering and Erosion
Section 1: Earth s Interior and Plate Tectonics Section 2: Earthquakes and Volcanoes Section 3: Minerals and Rocks Section 4: Weathering and Erosion Key Terms Crust Mantle Core Lithosphere Plate Tectonics
More information2 Igneous Rock. How do igneous rocks form? What factors affect the texture of igneous rock? BEFORE YOU READ. Rocks: Mineral Mixtures
CHAPTER 2 2 Igneous Rock SECTION Rocks: Mineral Mixtures BEFORE YOU READ After you read this section, you should be able to answer these questions: How do igneous rocks form? What factors affect the texture
More information4 th Grade PSI. Slide 1 / 107 Slide 2 / 107. Slide 3 / 107. Slide 4 / 107. Slide 5 / 107. Slide 6 / 107. The History of Planet Earth
Slide 1 / 107 Slide 2 / 107 4 th Grade PSI The History of Planet Earth 2015-11-10 www.njctl.org Slide 3 / 107 Slide 4 / 107 The History of Planet Earth The Structure of Earth Rock Layers Fossils and Relative
More information3. Bedrock from which entire geologic time period is missing between rock units 5 and 6? The fault most likely occurred after
Homework # 4 Relative Dating Name: Section: Date: 1. The cross section below represents a portion of Earth s crust. Letters through D are locations within the rock units. 5. The sequence of rock types
More informationAnswers: Internal Processes and Structures (Isostasy)
Answers: Internal Processes and Structures (Isostasy) 1. Analyse the adjustment of the crust to changes in loads associated with volcanism, mountain building, erosion, and glaciation by using the concept
More informationWriting Earth s History
Earths History Writing Earth s History How is Earths History like writing in your Journal? Everyday, something happens and, with a pen, it is written down in the pages of your journal. As you continue,
More informationDirected Reading A. Section: Relative Dating: Which Came First?
Skills Worksheet Directed Reading A Section: Relative Dating: Which Came First? Write the letter of the correct answer in the space provided. 1. Determining the age of objects or events in relation to
More informationTEACHER BACKGROUND KNOWEDGE. Minerals, Rocks and the Rock Cycle
TEACHER BACKGROUND KNOWEDGE Minerals, Rocks and the Rock Cycle Core Concepts Rocks in the Earth s crust vary in their form and structure based on process that made them. The constant changing of the form
More informationCity of Fort Collins: Geology Staff Training, June 2012
1 City of Fort Collins: Geology Staff Training, June 2012 Levels of Analysis Descriptive (What do you see, feel, hear, etc..) This rock is made of round grains of quartz. Interpretive-- (The detective
More informationGeology 12 FINAL EXAM PREP. Possible Written Response Exam Questions
Geology 12 FINAL EXAM PREP Possible Written Response Exam Questions Use this study guide to prepare for the written response portion of the final exam. Name FINAL EXAM - POSSIBLE WRITTEN RESPONSE QUESTIONS
More informationOhio s State Tests PRACTICE TEST GRADE 8 SCIENCE. Student Name
Ohio s State Tests PRACTICE TEST GRADE 8 SCIENCE Student Name The Ohio Department of Education does not discriminate on the basis of race, color, national origin, sex, religion, age, or disability in employment
More informationIgneous. Sedimentary Transformation by heat and pressure
Melting, cooling and hardening Turns you into an Igneous Rock! Limestone A Sedimentary Rock Erosion, deposition and cementation Turns you into a Sedimentary Rock! Transformation by heat and pressure Turns
More information4 Deforming the Earth s Crust
CHAPTER 7 4 Deforming the Earth s Crust SECTION Plate Tectonics BEFORE YOU READ After you read this section, you should be able to answer these questions: What happens when rock is placed under stress?
More informationVersion Date 6/26/17. Disciplinary Core Ideas (Framework)
1 Earth Is Rock 1 What's the Story of This Place? Students consider the history of Earth and begin to think about rock and landforms as a source of for Earth s past. An Earth tour provides a sense of the
More information2 Igneous Rock. How do igneous rocks form? What factors affect the texture of igneous rock? BEFORE YOU READ. Rocks: Mineral Mixtures
CHAPTER 4 2 Igneous Rock SECTION Rocks: Mineral Mixtures BEFORE YOU READ After you read this section, you should be able to answer these questions: How do igneous rocks form? What factors affect the texture
More informationEarth Science 11: Geologic Time Unit
Earth Science 11: Geologic Time Unit Text: Chapters 8 Lab: Exercise 6 Name Earth Science 11: Geologic Time Page 1 Geology 12: Geologic Time 8.1: The Geologic Time Scale Today, we know that Earth is approximately
More informationOhio s State Tests PRACTICE TEST LARGE PRINT GRADE 8 SCIENCE. Student Name
Ohio s State Tests PRACTICE TEST LARGE PRINT GRADE 8 SCIENCE Student Name The Ohio Department of Education does not discriminate on the basis of race, color, national origin, sex, religion, age, or disability
More informationGrade 7 Science Revision Sheet for third term final exam
Grade 7 Science Revision Sheet for third term final exam Material for the final exam : 1- Chapter 4 sections 1+2+3+4 [rock cycle + igneous rocks + sedimentary rocks + metamorphic rocks ] pages from the
More informationBack to the Big Question
5.1 Understand the 5.4 Question Explore Learning Set 5 Back to the Big Question What processes within Earth cause geologic activity? You now know a lot about patterns of volcanoes in your region and around
More informationLaw of Superposition Law of Superposition
History of Earth Relative Dating In the same way that a history book shows an order of events, layers of rock (called strata) show the sequence of events that took place in the past. Using a few basic
More informationMineral Element Compound Atom Crystal. Silicate Nonsilicate Inorganic Luster Streak. Cleavage Fracture Hardness Density Reclamation
6 th Grade Science Midterm Study Guide Due February 5 th * Midterm Date: February 9th (Tuesday) * Midterm will consist of 50 multiple choice questions (about 10 per chapter) YOU MUST DEFINE THE KEY TERMS
More informationDirected Reading. Section: Rocks and the Rock Cycle. made of a. inorganic matter. b. solid organic matter. c. liquid organic matter. d. chemicals.
Skills Worksheet Directed Reading Section: Rocks and the Rock Cycle 1. The solid part of Earth is made up of material called a. glacial ice. b. lava. c. rock. d. wood. 2. Rock can be a collection of one
More information!!!!! STOP!!!!! What is environmental geology? Earth as a closed system implies nearly everything is cycled, recycled
What is environmental geology?!!!!! STOP!!!!! Geology Study of rocks and minerals that comprise earth s surface and interior and the natural processes that shape the earth s surface and interior over all
More information!!!!! STOP!!!!! What is environmental geology?
!!!!! STOP!!!!! What is environmental geology? Geology Study of rocks and minerals that comprise earth s surface and interior and the natural processes that shape the earth s surface and interior over
More informationTOPIC 1: RELATIVE DATING ESSENTIAL QUESTION: HOW DO WE DETERMINE A ROCK S AGE BY THE SURROUNDING ROCKS?
TOPIC 1: RELATIVE DATING ESSENTIAL QUESTION: HOW DO WE DETERMINE A ROCK S AGE BY THE SURROUNDING ROCKS? TOPIC 1: RELATIVE DATING UNIFORMITARIANISM: THE IDEA THAT THE SAME FORCES HAVE BEEN AND CONTINUE
More informationEARTH S HISTORY. Geological Evolution
EARTH S HISTORY Geological Evolution EVIDENCE FOR EARTH S AGE ROCK LAYERS FOSSILS UNIFORMITARIANISM RELATIVE VS. EXACT DATING ROCK LAYERS Many thousands of sedimentary rock layers Takes thousands to millions
More informationAdapted by Karla Panchuk from Physical Geology by Steven Earle
Physical Geology, 3 rd Adapted Edition is used under a CC BY 4.0 International License Read this book online at http://openpress.usask.ca/physicalgeology/ Chapter 6. The Rock Cycle Adapted by Karla Panchuk
More informationGeoscience 001 Fall Rock Identification and Contextual Interpretation
Geoscience 00 Fall 2005 Rock Identification and Contextual Interpretation The purpose of this week s lab is to gain some more experience and practice in identifying rocks and then interpreting the geologic
More informationRelative Dating. How do we determine a rocks age by the surrounding rocks?
Relative Dating How do we determine a rocks age by the surrounding rocks? 1 Geologic History 2 Relative Dating Uniformitarianism - the idea that forces working on our planet today worked on our planet
More informationThe Rock and Fossil Record. Chapter 15 Sections 1-5
The Rock and Fossil Record Chapter 15 Sections 1-5 Objectives Page 123 CO: SWBAT describe how the science of geology has changed over the past 200 years. LO: SWBAT explain how studying the Earth s present
More informationEarth History 870:035
Earth History 870:035 Course goal: To describe the history of Earth and its inhabitants Most of Earth s history predates humanity, so it has not been observed Therefore, we will emphasize how scientists
More informationGEOL 104 Dinosaurs: A Natural History Geology Assignment. DUE: Mon. Sept. 19
GEOL 104 Dinosaurs: A Natural History Geology Assignment DUE: Mon. Sept. 19 Part I: Environments of Deposition Geologists can use various clues in sedimentary rocks to interpret their environment of deposition:
More informationRocks and the Rock Cycle. Banded Iron Formation
Rocks and the Rock Cycle Banded Iron Formation Rocks Big rocks into pebbles, Pebbles into sand. I really hold a million, million Rocks here in my hand. Florence Parry Heide How do rocks change? How are
More informationFaults, Fossils, Rocks and Minerals Review:
Faults, Fossils, Rocks and Minerals Review: 1. The preserved remains or traces of organisms that lived in the past are. - Fossils 2. How do Fossils form? - A dead organism becomes buried in sediment 3.
More informationName Class Date. Study Guide for 7 th Grade Final Exam (Semester One)
Name Class Date Study Guide for 7 th Grade Final Exam (Semester One) 1. What are the steps of the scientific method? Define the problem or question Form a hypothesis (MUST BE TESTABLE) o (identify variables)
More informationI. 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
How Earth s Rocks Were Formed 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 features of Earth were
More informationChapter 2. Early Geologists Tackle History's Mysteries
Chapter 2 Early Geologists Tackle History's Mysteries Nicolaus Steno and his Laws Danish (lived in Italy); 1638-1687 Pioneering studies of Italian strata Developed basic principles (laws) regarding age
More informationCross-Cutting Relationships Cross-Cutting and Sequencing Lab Earth Science Essentials-Advanced by Russ Colson
Cross-Cutting Relationships Cross-Cutting and Sequencing Lab Earth Science Essentials-Advanced by Russ Colson Introduction: It isn't possible to bring all of outdoors into the classroom, and stratigraphic
More informationIgneous magma cools crystals, holes Metamorphic heat & pressure wavy layers, foliation Sedimentary straight layers, rough, dull, fossils
First Semester Final Exam Study Guide Question Answer Illustration/Example List the three main types of rocks and draw a picture of each. Label the significant features. (Layers, crystals, holes, grains,
More informationLesson 4 Rocks Rock! Lesson Overview: Students will become familiar with rocks, minerals, and be introduced to the rock cycle.
Lesson 4 Rocks Rock! Lesson Overview: Students will become familiar with rocks, minerals, and be introduced to the rock cycle. Objectives: Students will be able to: 1. Explain the difference between rocks
More informationScience. Overview of Project: A new planet has just been discovered! Honors Project MP 4: New Planet s Core. DUE: June 4, 2013
Science Honors Project MP 4: New Planet s Core DUE: June 4, 2013 Overview of Project: A new planet has just been discovered! It revolved around a nearby star, just outside our solar system. An unmanned
More informationUnit E: Planet Earth. Topic 2: The Rock Cycle and Characteristics of Rocks
Unit E: Planet Earth Topic 2: The Rock Cycle and Characteristics of Rocks 1 2.1 Three Classes of Rocks: Igneous, Sedimentary, and Metamorphic A. How Rocks Are Formed B. Types of Rock 1. All rocks can be
More information1. minerals - A naturally occurring substance that takes a solid Crystal form and is made of only a single (one) type of compound
Science Name: Mr. G/Mrs. Kelly KEY Date: Study Guide - Lessons 5 and 6 Test Define the following terms: 1. minerals - A naturally occurring substance that takes a solid Crystal form and is made of only
More informationThe Earth s Structure
Planet Earth The Earth s Structure Crust the outermost and thinnest layer of Earth Mantle the layer of rock between the Earth s crust and its core - rocks are plastic soft and easily deformed The Earth
More informationThe Rocky Road Game. Sedimentary Rock. Igneous Rock. Start. Metamorphic Rock. Finish. Zone of Transportation. Weathering Way.
Sedimentary Rock Deposition Depot Zone of Transportation Transported: Advance 3 Weathering Way The Rocky Road Game Uplift: Advance 5 Lithification Lane Crystallization Crossway Submerge Detour take the
More informationQ. How do we know about the Earth s history? A. The ROCKS tell us stories
Q. How do we know about the Earth s history? A. The ROCKS tell us stories Q. What happened here? Q. What happened here? Q. What happened here? Vocabulary word: Uniformitarianism the scientific rule that
More informationObjectives: Define Relative Age, Absolute Age
S6E5. Students will investigate the scientific view of how the earth s surface is formed. c. Classify rocks by their process of formation. g. Describe how fossils show evidence of the changing surface
More information2. How do igneous rocks form? 3. How do sedimentary rocks form? 4. How do metamorphic rocks form?
Name: Class: Earth s History Test Review Packet Test: Monday, February 13, 2017 The Rock Cycle 1. Explain why it is called the rock CYCLE. Does it truly have a starting point or end point? 2. How do igneous
More informationLesson Learning Goal
Rock Dating Lesson Learning Goal 4/12 n I can identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive dating. Think About It... How old
More information1. In the block diagram shown here, which is the oldest rock unit?
Pre/Post GCI Name (print) 1. In the block diagram shown here, which is the oldest rock unit? 2. Referring to the same diagram as the previous question, which of the labeled rock units is the youngest?
More informationName Date Class. Directions: Use the diagram below to answer question Florida Progress Monitoring and Benchmark Assessments
b e n c h m a r k t e s t : e a r t h a n d s p a c e s c i e n c e Multiple Choice 1. Geologists obtain indirect evidence about Earth s interior by A measuring pressure differences at Earth s surface.
More information4 Deforming the Earth s Crust
CHAPTER 7 4 Deforming the Earth s Crust SECTION Plate Tectonics BEFORE YOU READ After you read this section, you should be able to answer these questions: What happens when rock is placed under stress?
More informationGeologic Time. Kentucky Geological Survey Modified McCann
Geologic Time Kentucky Geological Survey Modified McCann Procedure Plate tectonics Classroom activity #1 What is geologic time? Relative age dating Absolute age dating Classroom activity #2 T C What is
More informationName: Date: Use the following to answer question 2.
Name: Date: 1. Which of the following statements regarding the scientific method is false? A) A hypothesis must be agreed upon by more than one scientist. B) A theory is a hypothesis that has withstood
More informationEarth s Changing Surface Chapter 4
Name Hour Due Date Earth s Changing Surface Chapter (You do not need your book) Page 1 Fossils Summary Page 2 Traces of Tracks Page 3 Finding the Relative Age of Rocks Summary. Page - Finding the Relative
More informationPractice Test Rocks and Minerals. Name. Page 1
Name Practice Test Rocks and Minerals 1. Which rock would be the best source of the mineral garnet? A) basalt B) limestone C) schist D) slate 2. Which mineral is mined for its iron content? A) hematite
More informationL.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP
L.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP 1. Unless a series of sedimentary rock layers has been overturned, the bottom rock layer
More informationRock Cycle Reader s Theater
Rock Cycle Reader s Theater Characters Teacher1 Teacher 2 Student 1 Student 2 Student 3 Sedimentary Rock Crust Wind Water Ice Sediment 1 Sediment 2 Sediment 3 Metamorphic Rock The Rock Cycle Mantel Magma
More informationSTUDY GUIDE FOR MID-TERM EXAM KEY. Color, luster, cleavage, fracture, hardness, taste, smell, fluorescence, radioactivity, magnetism
STUDY GUIDE FOR MID-TERM EXAM KEY 1. In which type of rock are fossils most likely to be found? Sedimentary Rocks 2. Which mineral is easily identified by smell? Sulfur 3. Which natural resource makes
More informationToday you will be able to: Utilize the SEVEN rules of rock age identification to describe the geologic age of this rock sequence!
Mr. Sandomenico Welcome!!!! Today we will begin a new unit! The Earth s History!!!!! Today you will be able to: Utilize the SEVEN rules of rock age identification to describe the geologic age of this rock
More information1. In your own words, what is the Earth s crust?
The Structure of Earth Classwork Classwork #1 Name: 1. In your own words, what is the Earth s crust? 2. The Earth s surface became the way it is: A. only very recently. B. because of one event in history.
More informationWhy is quartz one of the most weathering-resistant minerals?
Why is it a poor idea to use limestone for tombstones in a wet hot area like the Amazon rainforest? A) Because limestone weathers at a very fast rate B) Because limestone weathers at a very low rate C)
More informationPlate Tectonics. Chapter 17. Great Idea: The entire Earth is still changing, due to the slow convection of soft, hot rocks deep within the planet.
Plate Tectonics Chapter 17 Great Idea: The entire Earth is still changing, due to the slow convection of soft, hot rocks deep within the planet. 1 Chapter Outline The Dynamic Earth Plate Tectonics: A Unifying
More information6. Relative and Absolute Dating
6. Relative and Absolute Dating Adapted by Sean W. Lacey & Joyce M. McBeth (2018) University of Saskatchewan from Deline B, Harris R, & Tefend K. (2015) "Laboratory Manual for Introductory Geology". First
More informationRAYMOND SIEVER Harvard University
E A R T H FOURTH EDITION FRANK PRESS National Academy of Sciences RAYMOND SIEVER Harvard University W. H. Freeman and Company New York Preface xiii Acknowledgments xviii PART I PROLOGUE CHAPTER 1 HISTORY
More informationRocks: Stony Stalwarts: Adapted from:
Rocks: Stony Stalwarts: Adapted from: http://science.nationalgeographic.com/science/earth/inside-the-earth/rocks-article/ Rocks are so common that most of us take them for granted cursing when we hit them
More information8 th Grade Science Tutoring. Earth Space, Ms. Winkle
8 th Grade Science Tutoring Earth Space, Ms. Winkle List of Topics PART ONE Atoms, molecules, elements, mixtures, compounds Density Physical vs chemical changes Weathering, Erosion, Deposition (include
More informationScience 20. Unit C: The Changing Earth. Assignment Booklet C1
Science 20 Unit C: The Changing Earth Assignment Booklet C FOR TEACHER S USE ONLY Summary Teacher s Comments Chapter Assignment Total Possible Marks 60 Your Mark Science 20 Unit C: The Changing Earth Assignment
More informationEarth s Interior HW Packet HW #1 Plate Tectonics (pages )
Name Earth s Interior HW Packet HW #1 Plate Tectonics (pages 676 683) 1. Is the following sentence true or false? According to the theory of plate tectonics, Earth s plates move about quickly on top of
More informationHafeet mountain. Rocks
Hafeet mountain Rocks There are several steps that lead to form the rocks Weathering Erosion Deposition Heat and pressure Weathering Ice (expand inside the rock fractures) Plants (grows through fractures
More informationEarth s Changing Surface
Earth s Changing Surface Fourth grade scientists are introduced to the scope of geologic time and learn about forces that change our Earth s surface. During their study, students use scientific modeling
More informationGrade 7 Earth/Space Posttest
Grade 7 Earth/Space Posttest Select the best answer to each question. 1. The three compositional layers of Earth are the core, the mantle, and the crust. Which phrase best describes the crust? A. the innermost
More information