LAB 5-2: MATCHING ROCK LAYERS

Similar documents
Page 1. Name:

ENVI.2030L Geologic Time

Geoscience 001 Fall Rock Identification and Contextual Interpretation

Geology 101 Lab Worksheet: Geologic Time

L.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP

9. DATING OF ROCKS, FOSSILS, AND GEOLOGIC EVENTS

Guided Notes Rocks & Minerals

1. The timeline below represents time on Earth from the beginning of the Paleozoic Era Ato the present B.

Unconformities, Geologic Time Scale, and Uniformitarianism. Ms. P Science 2016

3. Bedrock from which entire geologic time period is missing between rock units 5 and 6? The fault most likely occurred after

Geology Test Review Answers

Structural Geology Lab. The Objectives are to gain experience

Earth History Exam. The remains of an early dinosaur could be found at reference point A. A B. B C. C D. D. page 1

Earth Science - Lab #11 Geologic Time

GEOLOGIC HISTORY DIAGRAMS

Unit 6: Interpreting Earth s History

Modeling the Rock Cycle

Clues to Earth s Past

Practice 3rd Quarter Exam Page 1

NAME HOMEWORK ASSIGNMENT #3 MATERIAL COVERS CHAPTERS 8, 9, 10, 11

Before the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references.

Geology Stratigraphic Correlations (Lab #4, Winter 2010)

GCE AS/A level 1211/01 GEOLOGY GL1 Foundation Unit

TIME. Does not give the. Places events in sequencee 1 st, 2 nd, 3 rd. Gives a. exact date of an event. event. Radioactive Dating.

GEOLOGIC TIME AND GEOLOGIC MAPS

Objectives. Vocabulary. Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era, period, and epoch.

9. RELATIVE AND RADIOMETRIC AGES

Name: Date: Period: Page 1

Sedimentary Rocks. Rocks made of bits & pieces of other rocks.

1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite.

The Geology of Pacific Northwest Rocks & Minerals Activity 1: Geologic Time

Part 1: Observations for the Edwards Formation

November 3, SWABT interpret cross-sections with index fossils and unconformities to determine relative ages of rock layers.

Writing Earth s History

Answers: Internal Processes and Structures (Isostasy)

Regents Earth Science

GEOLOGY MEDIA SUITE Chapter 8

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

UNCONFORMITY. Commonly four types of unconformities are distinguished by geologists: a) Disconformity (Parallel Unconformity)

Before the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references.

Unit 5: Earth s History Practice Problems

Geology 101 Lab Worksheet: Geologic Structures

Earth s Changing Surface Chapter 4

Page 1. Name: Period: Date: WS Metamorphic Rocks. The diagram below represents a rock with a distorted layer structure.

Sedimentary Rocks. All sedimentary rocks begin to form when existing rocks are broken down into sediments Sediments are mainly weathered debris

CHAPTER 8 DETERMINING EARTH S AGE RELATIVE AND ABSOLUTE ROCK AGES. Loulousis

8. GEOLOGIC TIME LAST NAME (ALL IN CAPS): FIRST NAME: Instructions

Sedimentary Rocks, Stratigraphy, and Geologic Time

Determining geological ages

Part I. PRELAB SECTION To be completed before labs starts:

Rocks. Sedimentary Rocks. Before You Read. Read to Learn

Section I: Multiple Choice Select the best answer to each question. Mark your final answer on the answer sheet. (1 pt each)

2. How do igneous rocks form? 3. How do sedimentary rocks form? 4. How do metamorphic rocks form?

Earth History Teacher Rubrics and Directions

Structural Geology Lab. The Objectives are to gain experience

New Rock from the rock Cycle. Copyright 2010 Ryan P. Murphy

WEATHERING, EROSION & DEPOSITION STUDY GUIDE

Earth s History Packet 6

Happy Tuesday. Pull out a ½ sheet of paper

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

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

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

Relative Dating Exercises

GEOLOGIC TIME. Smith and Pun, Chapter 7 DETERMINING THE ORDER OF EVENTS

GEOLOGY GL1 Foundation Unit

GEOLOGICAL TIME / DATING TECHNIQUES

Review - Unit 2 - Rocks and Minerals

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

GY 112L Earth History

PLEASE DO NOT WRITE ON THIS QUIZ! Relative Dating and Stratigraphic Principles Quiz

C) Trenton limestone

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

N30 E-45 SE S25 E-10 SW N85 W-80 NE

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

Page 1. Weathering & Erosion by Mass Wasting Pre-Test. Name:

EES - Goal Rocks and Minerals

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

Core Description, Stratigraphic Correlation, and Mapping of Pennsylvanian Strata in the Appalachians

Name HW - Landscapes

GEOLOGIC MAPS PART II

4/4. K What I know about Sedimentary Rocks. W What I want to find out about Sedimentary Rocks Sunday, April 7, 13

Geologic Time. Geologic Events

* * * * *25

General Geology Lab #7: Geologic Time & Relative Dating

Answers. Rocks. Year 8 Science Chapter 8

Sedimentary Rocks. Rocks made of bits & pieces of other rocks.

Geohistory Review. Things you need to know:

Geology of the Hawaiian Islands

Lab 2 Geological Time and Fossil Samples

Geology 12 FINAL EXAM PREP. Possible Written Response Exam Questions

1. Base your answer to the following question on on the photographs and news article below. Old Man s Loss Felt in New Hampshire

Earth s History. Performance Indicator 1.2 Describe current theories about the origin of the universe and solar system. Standard 4 Key Idea 1

Chapter 09 Geologic Time

GEOLOGICAL TIME / DATING TECHNIQUES

Practice Packet Topic 6: Earth s History

Earth History 870:035

weathering and cooling and solidification compaction and cementation SEDIMENTARY ROCK

Cross-Cutting Relationships Cross-Cutting and Sequencing Lab Earth Science Essentials-Advanced by Russ Colson

WEDNESDAY, 27 MAY 1.00 PM 3.30 PM. Date of birth Day Month Year Scottish candidate number

Rocks and The Rock Cycle

Transcription:

NAME ATE NSTRUCTOR-------- PERO PARTNER UNT 5: Earths History LAB 5-2: MATCHNG ROCK LAYERS NTROUCTON: Geologists can determine the relative ages of the rock layers in a rock formation But how do they determine whether the rocks or geologic events occurring at one location are of the same age as those at another location? The process of showing that rocks or geologic events occurring at different locations are of the same age is called correlation Geologists have developed a system for correlating rocks by looking for similarities in composition and rock layer sequences at different locations Certain fossils, called index fossils, existed for a very short time and were distributed over a large geographic area They aid the geologist in correlating sedimentary rock layers OBECTVE: You will be able to construct a geologic history of a region by observing rock layers in different localities VOCABULARY: absolute age: index fossil: correlation: PROCEURE A: The first set of four diagrams represent four outcrops at different locations 1 Reconstruct the complete sequence of events Assume that the oldest rocks are on the bottom and the youngest are on top 2 raw in the layers on the appropriate column of the Report Sheet PROCEURE B: The second set of diagrams identifies four types of index fossils and shows four columns of fossil bearing rock strata Assume overturning has not occurred l Reconstruct the complete sequence of events and draw the layers (with the fossils if present) on the appropriate column of your Report Sheet 2 By referring to your Reference Tables, identify any layer for which you have enough evidence to determine its age On the Report Sheet, label its age and period/epoch The abbreviation mybp" stands for millions of years before present t may be expressed as a range of several million years 191

A: OUTCROPS FROM FOUR LOCATONS A 8 c KEY ++t tt + t t t + + t t+ + t + " ::--=-=- -- - - - - -----=- - - - -- - - - : : : :::::::::: ::::::::::::::::: : ;; g;en;m;ggg== u 1iff rnhviw W1i il\1 --- --- - -=-- ----- --- - - - -- --= - - / [ll; - Contact Metamorphism Gneiss Basalt Conglomerate Sandstone Siltstone Shale Limestone Rock Salt NEX FOSSLS OF FFERENT GEOLOGC PEROS Q PECTEN (Oligocene Epoch to Recent) CRNO (Mississippian l AMMONTE (Cretaceous TRLOBTE (evonian B: ROCK STRATA CONTANNG NEX FOSSLS :_ " : : : : : : A B c 192

Procedur9 A REPORT SHEET Procedure 8 -- - ate mybp l Geologic Period 193 l l l

PROCEURE C: The third set of diagrams represent three different outcrops Using the rock type of the strata correlate the columns 1 raw lines representing equivalent boundaries between rock layers from one column to the next 2 Reconstruct the complete column in the blank column Assume that the oldest rocks are on the bottom and the youngest are on the top 3 raw in thick lines on columns 1,2, and 3 identifying the locations of unconformities RECONSTRUCTE COLUMN 1 :-: : -:: ::; ::-: - : f : :, 2 3 : : : :: > ; : : ::: : : : : : :: 194

SCUSSON QUESTONS: (Answer in Complete Sentences) 1 Explain why some rock layers can be missing from the sequence in some outcrops 2 What does a field geologist look for in rock outcrops to help identify the different rock layers? 3 Why is it easier for you to correlate diagrams than it is for a geologist in the field to reconstruct a sequence of events? 4 n Procedure B, what is the youngest possible age of the rock stratum at the very bottom of the geologic column? 5 n Procedure B, how many years are represented between the top and bottom fossil bearing layers? 6 Explain why you can find the same type of fossil in different types of rock strata 7 Explain how it is possible that a given type of fossil may be found in a rock stratum at one outcrop, but missing from that same layer at another outcrop 8 n Procedure C, what is a reason that the limestone in column 1 is thinner than the limestone in column 2? 9 According to the appearance of the right side of each column in Procedure C, which rock type appears to be the least resistant to weathering and erosion? CONCLUSON: Why is it necessary to observe the rock layers of several different localities in order to obtain a complete sequence of events? 195