GY 112L Lab Assignment 8 Paleozoic Lab 2

Size: px
Start display at page:

Download "GY 112L Lab Assignment 8 Paleozoic Lab 2"

Transcription

1 Name: Grade /100 (+5 bonus) Percent: GY 112L Lab Assignment 8 Paleozoic Lab 2 Note: There are a lot of specimens to look at in this weeks lab. It is probably best for you to look at the physical specimens first and do the written questions last. This way if you run out of lab time, you ll be able to finish off the rest of the lab at home. Part 1: Fossils Sponges (Phylum Porifera; Cambrian to Recent) and Stromatolites (Archean Recent) Specimen 8-1a: Astraeospongia sp. (Silurian); Specimen 8-1b: stromatolite (Paleozoic); Specimen 8-1c: Corynella sp. (Cretaceous) Why do sponges like specimen 8-1a have spicules? Specimen 8-1c is an excellent fossilized sponge. What characteristic(s) tell you that it is a sponge? (hint: examine the specimen with your hand lens) [3 points] Specimen 8-1b is a fine example of a Paleozoic stromatolite. Where are the oldest stromatolites on the Earth found? (Refer to your web notes for the answer). [3 points] Corals: (Phylum Cnidaria; Cambrian to Recent) Specimen 8-2a: Streptelasma sp. Ord.- Dev., Specimen 8-2b: Heliophyllum sp. Dev., Specimen 8-2c: Favosites sp. Ord Perm., Specimen 8-2d: unknown tabulate coral HY-73 Which specimen(s) are colonial corals? [3 points] Which specimen(s) are solitary corals? [3 points] A possible internet research question: How do modern coral propagate? [5 points] i

2 Bryozoans (Phylum Bryozoan, Ordovican-Recent) Specimen 8-3a: Dekayella sp., Ord., Specimen 8-3b: Hallopora sp. Ord-Dev., Specimen 8-3c Archimedes sp. Miss-Perm. Some Bryozoans are twig like while others are lacy; however, they all share some common charcteristics. What are they? [5 points] Specimen 8-3c is called Archimedes? Why is this a good name for this beastie? (Hint who was Archimedes and what did he do?) [5 points] More Drawing 101 Draw any Two of the organisms in the lab today. Use the box below and the one at the top of the next page for your sketches. Remember to use pencil, and add shading where possible. Be sure to add scales (use cm not inches) to your diagrams. If you are unclear as to how you go about doing this, ask us. [10 points each; 20 total] Name of Specimen: Specimen Number: Scale ii

3 Name of Specimen: Specimen Number: Scale Want some additional credit? Draw another (different) beastie for 5 bonus points Name of Specimen: Specimen Number: Scale iii

4 Part 2: Niagara Falls Rock Suite Background: The Niagara Falls area (southern Ontario, Canada and northern New York State; Figure 8-8) is underlain by a combination of siliciclastic and carbonate rock units that range in age from the Ordovician to the Silurian. There are numerous facies changes within the strata and even a few unconformities. The neat thing about the rocks is their exposure. Rocky outcrops can be found all around the Niagara Falls area. In fact, you can trace individual beds for a couple of hundred kilometers from northern New York State to the tip of the Bruce Peninsula in Ontario. For this lab, you will see rocks, maps, and stratigraphic sections. Stratigraphy. Figure 8-9 at the top of the next page is a stratigraphic column for the northern portion of the United States (Including parts of Canada) from Michigan to New York. It covers the Cambrian-Silurian intervals of geological time. It initially looks pretty complex, but do not panic! It isn't all that difficult to interpret once you get your eyes in focus. The extreme left columns are time intervals. Here you will spot your old friends the Cambrian (Camb.) Ordovician and Silurian. You will also see the divisions Early, Middle and Late. A lot of the other terms (Niagaran, Llandoverian etc.) are epochs or other divisions that we do not have to worry about in GY 112/112L. The rest of the columns relate the stratigraphy at specific areas. Figure 8-8: Paleogeographic map of southern Ontario, New York and Pennsylvania during the Wenlockian Epoch. From Cheel, R.J., Sedimentology and depositional environments of Silurian Strata of the Niagara Escarpment, Ontario and New York. iv

5 Figure 8-9: A portion of Paleozoic stratigraphy covering the area around Niagara Falls From Cheel, R.J., Sedimentology and depositional environments of Silurian Strata of the Niagara Escarpment, Ontario and New York. The Niagara region is the second column from the right. The names that occur in the rows within each column are formation etc. names. Refer to the Niagara area column to answer the next 6 questions. What age is the Rochester Formation? [3 points] What age is the Queenston Formation? [3 points] To which group does the Whirlpool Formation belong? [3 points] What happens to the Queenston Formation from Windsor-Sarnia to W. New York? [4 points] v

6 What do you think the black areas represent across the stratigraphic columns? [4 points] Why are the Silurian black areas thicker at Algonquin Arch than at other geographical regions in the area? (Hint: Think time and topography before you ask for help). [4 points] Rock Suites. Figure 8-10 to the right is a sedimentary section through the rocks that underlay Niagara falls. Rock samples 8-4 through 8-6 (locations shown on the figure) come from this section. Figure modified from Cheel, R.J., Sedimentology and depositional environments of Silurian Strata of the Niagara Escarpment, Ontario and New York. 8-6 Rock Specimen 8-4: Rochester Formation. What is class of sedimentary rock is this specimen? [2 points] 8-5 What is the name of this sedimentary rock [3 points] Rock Specimen 8-5: Gasport Formation. Some 8-4 people clump this formation into the Lockport Group. Regardless of what you call it, this rock and the Rochester Formation below are the reason why we have Niagara Falls. What properties of the Gasport/Lockport Formation coupled with the stratigraphic relationships between the formation helped to produce Niagara Falls? (Hint: consider the stratigraphy in Figure What are the black layers composed of and how do they differ from the white layers?) [3 points] vi

7 Rock Specimen 8-6: Goat Island Formation. This is a fine-grained sedimentary rock with round chert nodules. What is class of sedimentary rock is this specimen? [2 points] What is the name of this sedimentary rock [3 points] Look at the rock with your hand lens. Geologists often use the term "sucrosic" to describe dolostones. Why do they do this and do you agree with its usage here? [3 points] The Falls. The figure below is a cartoon of Niagara Falls viewed from the air. From Cheel, R.J., Sedimentology and depositional environments of Silurian Strata of the Niagara Escarpment, Ontario and New York. Given that the Peace River Bridge is 500 m long, determine the rate of retreat of the Horseshoe (Canadian) Falls from: 1378 to 1678: m/year [3 points] 1842 to 1927: m/year [3 points] vii

8 Name: Last Question: Without Niagara Falls, it s unlikely that the cities of Niagara Falls (one in Canada, the other in the US) would ever have become the Honeymoon Capitals of the world. No hotels would have located here. All the wax museums, strip clubs and other el- d to go somewhere else. With the exception of cheapo tourist attractions would have ha Orlando, Las Vegas and other existing tourist traps, where might these eyesores have gone and why? (Note: the funnier your answer, the better your grade). [10 points] Notes viii

GY 112L: Earth History Lab

GY 112L: Earth History Lab UNIVERSITY OF SOUTH ALABAMA GY 112L: Earth History Lab Week 11 Paleozoic Part 2 Instructor: Dr. Douglas W. Haywick Today s Agenda The Paleozoic Part 2 (Lab 8 exercises) 1) Sponges & Stromatoporoids 2)

More information

GY 112L Lab Assignment 12 Cenozoic Rocks and Fossils

GY 112L Lab Assignment 12 Cenozoic Rocks and Fossils Name: Grade /100 +10 bonus Percent: GY 112L Lab Assignment 12 Cenozoic Rocks and Fossils Note: This is the first and only one of the GY 112 labs that deals with the Cenozoic Era. The lab is broken up into

More information

Shield was above sea-level during the Cambrian and provided the sediment for the basins.

Shield was above sea-level during the Cambrian and provided the sediment for the basins. Name: Answers Geology 1023 Lab #8, Winter 2014 Platforms and Paleozoic life-forms Lab day: Tu W Th 1. Schematic geologic cross-sections A-B and C-D (shown below) cross the edge of the continental platform

More information

Lecture 24: Paleozoic 1:

Lecture 24: Paleozoic 1: UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 24: Paleozoic 1: Laurentia Instructor: Dr. Douglas W. Haywick Last Time (before the exam) The Cambrian Explosion A) Why a Cambrian explosion B)

More information

GY 111: Physical Geology

GY 111: Physical Geology UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 21: Rock Deformation Instructor: Dr. Douglas W. Haywick Last Time A) How long is long? B) Geological time divisions Web notes 20 Geological

More information

Structural Geology Lab. The Objectives are to gain experience

Structural Geology Lab. The Objectives are to gain experience Geology 2 Structural Geology Lab The Objectives are to gain experience 1. Drawing cross sections from information given on geologic maps. 2. Recognizing folds and naming their parts on stereoscopic air

More information

The Niagara Escarpment extends from western New York, through the GTA all the way up to Manitoulin Island and into Michigan and Wisconsin.

The Niagara Escarpment extends from western New York, through the GTA all the way up to Manitoulin Island and into Michigan and Wisconsin. is southern Ontario s most prominent topographic feature, extending more than 500 kilometres from western New York, through Niagara Falls and the western part of the Greater Toronto Area (GTA), and north

More information

Section 7. Reading the Geologic History of Your Community. What Do You See? Think About It. Investigate. Learning Outcomes

Section 7. Reading the Geologic History of Your Community. What Do You See? Think About It. Investigate. Learning Outcomes Chapter 3 Minerals, Rocks, and Structures Section 7 Reading the Geologic History of Your Community What Do You See? Learning Outcomes In this section, you will Goals Text Learning Outcomes In this section,

More information

GY 112 Lecture Notes Significance of Fossils: Paleogeography Interpretations

GY 112 Lecture Notes Significance of Fossils: Paleogeography Interpretations GY 112 Lecture Notes D. Haywick (2006) 1 GY 112 Lecture Notes Significance of Fossils: Paleogeography Interpretations Lecture Goals: A) What is paleogeography? B) How it works (Late Cambrian fantasy example)

More information

9. DATING OF ROCKS, FOSSILS, AND GEOLOGIC EVENTS

9. DATING OF ROCKS, FOSSILS, AND GEOLOGIC EVENTS LAST NAME (IN CAPS): FIRST NAME: Instructions: 9. DATING OF ROCKS, FOSSILS, AND GEOLOGIC EVENTS Refer to Laboratory 8 in your Lab Manual on pages 207-226 to answer the questions in this work sheet. Your

More information

CLIMATE CHANGE, CATASTROPHE AND THE TIDES OF HISTORY. 1. CLIMATE THE LONG VIEW.

CLIMATE CHANGE, CATASTROPHE AND THE TIDES OF HISTORY. 1. CLIMATE THE LONG VIEW. LL Innis / 3ALB 2018 CLIMATE CHANGE, CATASTROPHE AND THE TIDES OF HISTORY. 1. CLIMATE THE LONG VIEW. Climate has controlled our evolution, our spread around the globe, and our social, political, economic

More information

SAMPLE QUESTIONS FOR GEOLOGY 103, TEST 1

SAMPLE QUESTIONS FOR GEOLOGY 103, TEST 1 SAMPLE QUESTIONS FOR GEOLOGY 103, TEST 1 The correct answers are listed at the bottom (no peeking!). These questions are to give you an idea of the type of questions that will be asked. They are not a

More information

Structural Geology Lab. The Objectives are to gain experience

Structural Geology Lab. The Objectives are to gain experience Geology 2 Structural Geology Lab The Objectives are to gain experience 1. Drawing cross sections from information given on geologic maps. 2. Recognizing folds and naming their parts on stereoscopic air

More information

Shale Gas Opportunities in Southern Ontario an Update

Shale Gas Opportunities in Southern Ontario an Update Shale Gas Opportunities in Southern Ontario an Update Terry Carter, Ministry of Natural Resources, London, ON Lee Fortner, Ministry of Natural Resources, London, ON Catherine Béland-Otis, Ontario Geological

More information

Devil s Punchbowl -Virtual Field Trip-

Devil s Punchbowl -Virtual Field Trip- Devil s Punchbowl -Virtual Field Trip- School of GEOGRAPHY & GEOLOGY Carolyn Eyles & Susan Vajoczki Prepared by Zachary Windus and Liz Kenny From McMaster University take Main Street West towards Ancaster.

More information

A Journey Back in Time

A Journey Back in Time A Trip Through Geologic Time TEACHER NOTES Lab zonetm A Journey Back in Time The following steps will walk you through the. Use the hints and detailed directions as you guide your students through planning,

More information

Geology Stratigraphic Correlations (Lab #4, Winter 2010)

Geology Stratigraphic Correlations (Lab #4, Winter 2010) Name: Answers Reg. lab day: Tu W Th Geology 1023 Stratigraphic Correlations (Lab #4, Winter 2010) Introduction Stratigraphic correlation is the process of comparing rocks at one locality with related rocks

More information

Geology 101 Lab Worksheet: Geologic Time

Geology 101 Lab Worksheet: Geologic Time Geology 101 Lab Worksheet: Geologic Time Name: Refer to the Geologic Time Lab for the information you need to complete this worksheet (http://commons.wvc.edu/rdawes/g101ocl/labs/geotimelab.html). All calculations

More information

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

Unconformities, Geologic Time Scale, and Uniformitarianism. Ms. P Science 2016 Unconformities, Geologic Time Scale, and Uniformitarianism Ms. P Science 2016 Do Now due tomorrow! 1. Compare and contrast relative dating to absolute dating. 2. The Law of Superposition states that younger

More information

Biology. Slide 1 of 40. End Show. Copyright Pearson Prentice Hall

Biology. Slide 1 of 40. End Show. Copyright Pearson Prentice Hall Biology 1 of 40 2 of 40 Fossils and Ancient Life What is the fossil record? 3 of 40 Fossils and Ancient Life The fossil record provides evidence about the history of life on Earth. It also shows how different

More information

L.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 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 information

GY 112L Earth History

GY 112L Earth History GY 112L Earth History Lab 2 Vertical Successions and Sequences of Events GY 112L Instructors: Douglas Haywick, James Connors, Mary Anne Connors Department of Earth Sciences, University of South Alabama

More information

Lecture Outline Friday Feb. 21 Wednesday Feb. 28, 2018

Lecture Outline Friday Feb. 21 Wednesday Feb. 28, 2018 Lecture Outline Friday Feb. 21 Wednesday Feb. 28, 2018 Questions? Key Points for today What are the 5 relative age dating principles and how do you apply the principles to determine a geologic history

More information

Quiz Three (9:30-9:35 AM)

Quiz Three (9:30-9:35 AM) Quiz Three (9:30-9:35 AM) UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 7 & 8: Dating Instructor: Dr. Douglas W. Haywick Last Time 1. William Smith and Water 2. Stratigraphic Principles 3.

More information

Field trip to Racine Reef Complex, Thornton Quarry, Illinois

Field trip to Racine Reef Complex, Thornton Quarry, Illinois Field trip to Racine Reef Complex, Thornton Quarry, Illinois Primary objectives for this fieldtrip 1) Collect and identify the fossils of the Racine Reef Complex. 2) Discuss procedures for collecting fossil

More information

Geological Time How old is the Earth

Geological Time How old is the Earth Geological Time How old is the Earth How old is everything? Universe? Universe ~ 14 Billion Years Old Milky Way Galaxy? Milky Way Galaxy - 10 Billion Years Old Solar System? Solar System -4.6 Billion Years

More information

LANDFORM REGIONS IN CANADA. Classroom Notes and Descriptions

LANDFORM REGIONS IN CANADA. Classroom Notes and Descriptions LANDFORM REGIONS IN CANADA Classroom Notes and Descriptions Landform Regions in Canada There are eight distinct landforms in Canada: Western Cordillera Region Interior Plains Canadian Shield Hudson Bay

More information

GY 112 Lecture Notes Significance of Fossils: Paleoenvironmental Interpretations

GY 112 Lecture Notes Significance of Fossils: Paleoenvironmental Interpretations GY 112 Lecture Notes D. Haywick (2006) 1 GY 112 Lecture Notes Significance of Fossils: Paleoenvironmental Interpretations Lecture Goals: A) The oceans today B) Estimating water depths C) Adaptations to

More information

Lab 4: Structures and Geologic Maps

Lab 4: Structures and Geologic Maps Key Questions: GEOL 1311 Earth Science Lab 4 Structures and Geologic Maps What shapes do rock bodies take in the Earth? How do two-dimensional visualizations of the Earth, such as maps and cross-sections

More information

5 Time Marches On. TAKE A LOOK 1. Identify What kinds of organisms formed the fossils in the picture?

5 Time Marches On. TAKE A LOOK 1. Identify What kinds of organisms formed the fossils in the picture? CHAPTER 6 5 Time Marches On SECTION The Rock and Fossil Record BEFORE YOU READ After you read this section, you should be able to answer these questions: How do geologists measure time? How has life changed

More information

GY 112 Lab Assignment 2 Vertical Succession and Sequence of Events Cartoons

GY 112 Lab Assignment 2 Vertical Succession and Sequence of Events Cartoons Name: Grade /100+5 bonus GY 112 Lab Assignment 2 Vertical Succession and Sequence of Events Cartoons Note: In many of the sequence of events exercises you will be asked to determine the exact order in

More information

Quiz Nine (9:30-9:35 AM)

Quiz Nine (9:30-9:35 AM) Quiz Nine (9:30-9:35 AM) UNIVERSITY OF SOUTH ALAAMA GY 112: Earth History Lecture 25: Paleozoic 2: More Laurentia! Instructor: Dr. Douglas W. Haywick Last Time The Paleozoic of North America 1) Laurentian

More information

Neoarchean to Mesoarchean Ga

Neoarchean to Mesoarchean Ga Name: Answers Geology 1023 Lab #7, Winter 2014 Shields & Precambrian life forms Lab day: Tu W Th Shields are the oldest (and most stable) parts of the continental masses. They consist of rocks of Precambrian

More information

Field Trip to Tempe Butte

Field Trip to Tempe Butte Synopsis Field Trip to Tempe Butte So far you have been identifying rocks and mapping their locations without actually going there. Now it is your chance to put it all together and see real rocks out in

More information

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

Core Description, Stratigraphic Correlation, and Mapping of Pennsylvanian Strata in the Appalachians Core Description, Stratigraphic Correlation, and Mapping of Pennsylvanian Strata in the Appalachians The remaining laboratory sessions for the semester will be collected into a series of exercises designed

More information

GEOL 02 Lab 9 Field Trip III Centerville Stratigraphic Section Name: Date:

GEOL 02 Lab 9 Field Trip III Centerville Stratigraphic Section Name: Date: Name: Date: Team Name: Team Members: Our goal today is to describe the sedimentary lithostratigraphic section of exposed bedrock along the road near Centerville Beach, interpret the depositional environment,

More information

Field Trip 1 Tunnel Mill, Vernon, Indiana: Waldron Shale

Field Trip 1 Tunnel Mill, Vernon, Indiana: Waldron Shale Geol G308 Paleontology and Geology of Indiana Name: Field Trip 1 Tunnel Mill, Vernon, Indiana: Waldron Shale On this trip we will visit Tunnel Mill, which is located just south of Vernon, Indiana in the

More information

OIL AND GAS PLAYS OF THE MICHIGAN BASIN, SOUTHERN ONTARIO. Terry Carter, Consulting Geologist London, Ontario

OIL AND GAS PLAYS OF THE MICHIGAN BASIN, SOUTHERN ONTARIO. Terry Carter, Consulting Geologist London, Ontario OIL AND GAS PLAYS OF THE MICHIGAN BASIN, SOUTHERN ONTARIO Terry Carter, Consulting Geologist London, Ontario 1 Ontario Petroleum Industries Oil and Natural Gas 1250 oil wells, 1200 gas wells, annual production

More information

MOR TIME TEACHERS. ONCE UPON A TIME Activity Overview BIG IDEA

MOR TIME TEACHERS. ONCE UPON A TIME Activity Overview BIG IDEA MOR TIME 04 Activity Overview BIG IDEA OBJECTIVE BACKGROUND The geologic time scale can be challenging for students to understand. This activity explores how scientists divide the Earth s long history

More information

2 Aggregates in Indiana

2 Aggregates in Indiana 2 Aggregates in Indiana Origin of Aggregates Gravel and Natural Sands Crushed Stone Slag Distribution of Aggregates Glacial Deposits Bedrock Deposits Aggregate Types Natural Aggregates Artificial Aggregates

More information

GY 112L Lab Assignment 5 Modes of Fossil Preservation

GY 112L Lab Assignment 5 Modes of Fossil Preservation Name: Grade /100 (+5 bonus) Percent: GY 112L Lab Assignment 5 Modes of Fossil Preservation Note: In this lab we will begin to look at fossilized animals, plants, and their traces. You will soon become

More information

17-1 The Fossil Record Slide 1 of 40

17-1 The Fossil Record Slide 1 of 40 1 of 40 Fossils and Ancient Life Fossils and Ancient Life Paleontologists are scientists who collect and study fossils. All information about past life is called the fossil record. The fossil record includes

More information

Timing of Geologic Events. Geologic Time Terms. Laws / Principles of Stratigraphy

Timing of Geologic Events. Geologic Time Terms. Laws / Principles of Stratigraphy Geologic Time Terms Hadean Archean Proterozoic Phanerozoic Paleozoic Mesozoic Cenozoic(Tertiary) Cambrian Unconformity Angular unconformity Half-life Alpha particle Beta particle Gamma ray Neutron UT How

More information

GEOL 3700 STRUCTURE AND TECTONICS LABORATORY EXERCISE 3

GEOL 3700 STRUCTURE AND TECTONICS LABORATORY EXERCISE 3 GEOL 3700 STRUCTURE AND TECTONICS LABORATORY EXERCISE 3 Goals: 1. Improve your map-reading and map-making skills. 2. Learn to generate and interpret structure contour maps. 3. Learn to generate and interpret

More information

Chapter 8 TIMING THE GEOLOGIC RECORD

Chapter 8 TIMING THE GEOLOGIC RECORD Chapter 8 Fossils (cont.): Petrified Forest, Arizona. These ancient logs are millions of years old. Their substance was completely replaced by silica, which preserved all the original details of form.

More information

Stratigraphic Cross-Section

Stratigraphic Cross-Section Stratigraphic cross-sections are used to show stratigraphic relationships of strata along some path. They differ from structural cross-sections in three ways. First, their goals differ. Stratigraphic cross-sections

More information

Geologic Time. Geologic Events

Geologic Time. Geologic Events Geologic Time Much of geology is focused on understanding Earth's history. The physical characteristics of rocks and minerals offer clues to the processes and conditions on and within Earth in the past.

More information

2 Eras of the Geologic Time Scale

2 Eras of the Geologic Time Scale CHAPTER 8 2 Eras of the Geologic Time Scale SECTION The History of Life on Earth BEFORE YOU READ After you read this section, you should be able to answer these questions: What kinds of organisms evolved

More information

GEOLOGIC HISTORY DIAGRAMS

GEOLOGIC HISTORY DIAGRAMS NAME: Log onto YouTube and search for jocrisci channel. GEOLOGIC HISTORY DIAGRAMS (Video 6.1) 1. Given a geologic cross section, you must be able to recognize folding, faulting, intrusions, unconformities,

More information

Fossils: evidence of past life

Fossils: evidence of past life Fossils: evidence of past life Remains or traces of prehistoric life Petrified Cavities and pores are filled with precipitated mineral matter Petrified Formed by replacement Cell material is removed and

More information

GY 112: Earth History. Fossils Part:

GY 112: Earth History. Fossils Part: UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Fossils Part: Telling Time Predicting Paleoenvironments Instructor: Dr. Douglas W. Haywick Last Time 1. Chronostratigraphy versus biostratigraphy 2. Paleontological

More information

GEOLOGY AND MINERAL RESOURCES OF INDIAN RESERVE 26

GEOLOGY AND MINERAL RESOURCES OF INDIAN RESERVE 26 ) 41HI3NW94I4 I R NO 26 1*A1 MANITOULIN ISLAND 010 -f?;. GEOLOGY AND MINERAL RESOURCES OF INDIAN RESERVE 26 September 16, 1975 D. G. Innes, Resident Geologist Sudbury District Ministry of Natural Resources

More information

William Smith Exhibition A Level Geology Challenge

William Smith Exhibition A Level Geology Challenge William Smith Exhibition A Level Geology Challenge RELEVANT TO GEOLOGY GCE A LEVEL SYLLABUS About this resource This resource for A Level has been written to support the William Smith Maps exhibition,

More information

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

1. The timeline below represents time on Earth from the beginning of the Paleozoic Era Ato the present B. Name Roy G Biv 1. The timeline below represents time on Earth from the beginning of the Paleozoic Era Ato the present B. Which numbered position best represents the time when humans first appeared in the

More information

Age of Earth/Geologic Time. Vocabulary

Age of Earth/Geologic Time. Vocabulary Age of Earth/Geologic Time Vocabulary Big Ideas Geologic Time Earth Structures Identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive

More information

City of Fort Collins: Geology Staff Training, June 2012

City 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 information

Geology 101 Lab Worksheet: Geologic Structures

Geology 101 Lab Worksheet: Geologic Structures Name: Geology 101 Lab Worksheet: Geologic Structures Refer to the Geologic Structures Lab for the information you need to complete this worksheet (http://commons.wvc.edu/rdawes/g101ocl/labs/structurelab.html).

More information

Date: TEN UNIT. Earth. History. and

Date: TEN UNIT. Earth. History. and Name: Date: UNIT TEN Geologic Time and Earth History *Dedicated to: Name: Date: ABSTRACTT AND RATIONALE The Earth is very old 4.5 billion years or more according to scientific estimates. Most of the evidence

More information

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

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

More information

Geoscience 001 Fall Rock Identification and Contextual Interpretation

Geoscience 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 information

Remains or traces of prehistoric life

Remains or traces of prehistoric life Fossils: evidence of past life Remains or traces of prehistoric life Petrified Cavities and pores are filled with precipitated p mineral matter Petrified Formed by replacement Cell material is removed

More information

Rock cycle diagram. Principle of Original Horizontality. Sediment is deposited horizontally

Rock cycle diagram. Principle of Original Horizontality. Sediment is deposited horizontally Geologic Time Rock cycle diagram Leaves of History Chapter 21 Lateral Continuity Principle of Original Horizontality Sediment is deposited horizontally Principle of Superposition Oldest rock A Younger

More information

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 History Exam. The remains of an early dinosaur could be found at reference point A. A B. B C. C D. D. page 1 Name: Date: 1. Base your answer(s) to the following question(s) on the Earth Science Reference Tables and your knowledge of Earth science. The accompanying cross section shows undisturbed sedimentary bedrock.

More information

Siliciclastic Hand Samples

Siliciclastic Hand Samples Describing siliciclastic rocks in hand sample Many aspects of siliciclastic rocks are best described in thin section, yet you will often be faced with the necessity of describing them in hand sample. That

More information

GEOLOGIC MAPS PART II

GEOLOGIC MAPS PART II EARTH AND ENVIRONMENT THROUGH TIME LABORATORY - EES 1005 LABORATORY FIVE GEOLOGIC MAPS PART II Introduction Geologic maps of orogenic belts are much more complex than maps of the stable interior. Just

More information

Geologic Time. Decoding the Age of our Planet & North Carolina

Geologic Time. Decoding the Age of our Planet & North Carolina Geologic Time Decoding the Age of our Planet & North Carolina The Geologic Time Scale Objectives Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era,

More information

GY 112L Earth History

GY 112L Earth History GY 112L Earth History Lab 6 Biostratigraphy and Foraminifera GY 112L Instructors: Douglas Haywick, James Connors, Mary Anne Connors Department of Earth Sciences, University of South Alabama Fifth Edition:

More information

HISTORICAL GEOLOGY. Relative & Absolute age, fossils and geologic time

HISTORICAL GEOLOGY. Relative & Absolute age, fossils and geologic time HISTORICAL GEOLOGY Relative & Absolute age, fossils and geologic time Historical Geology A. Measuring Time 1. Relative Time (Relative Age) Measurement of time using comparison. No numbers used; uses words

More information

Read It! Station Directions

Read It! Station Directions Read It! Station Directions Each member of the group will read the passage and answer the questions from the task cards on the lab sheet in the Read It! section. It is important to remember that the answers

More information

Cross-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 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 information

Relative Dating. The Rock Cycle. Key Concept Scientists can interpret the sequence of events in Earth s history by studying rock layers.

Relative 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 information

Name. GEOL.5220 Structural Geology Faults, Folds, Outcrop Patterns and Geologic Maps. I. Properties of Earth Materials

Name. GEOL.5220 Structural Geology Faults, Folds, Outcrop Patterns and Geologic Maps. I. Properties of Earth Materials I. Properties of Earth Materials GEOL.5220 Structural Geology Faults, Folds, Outcrop Patterns and Geologic Maps Name When rocks are subjected to differential stress the resulting build-up in strain can

More information

GY 112 Lecture Notes Proterozoic Life forms

GY 112 Lecture Notes Proterozoic Life forms GY 112 Lecture Notes D. Haywick (2006) 1 Lecture Goals: A) Eukaryote Life forms (Acritarchs) B) Metazoans (Ediacaran Fauna) GY 112 Lecture Notes Proterozoic Life forms Textbook reference: Levin 7 th edition

More information

Rock cycle diagram. Relative dating. Placing rocks and events in proper sequence of formation Deciphering Earth s history from clues in the rocks

Rock cycle diagram. Relative dating. Placing rocks and events in proper sequence of formation Deciphering Earth s history from clues in the rocks Geologic Time Rock cycle diagram Leaves of History Chapter 21 Modern geology Uniformitarianism Fundamental principle of geology "The present is the key to the past Relative dating Placing rocks and events

More information

Geologic Time Scavenger Hunt

Geologic Time Scavenger Hunt Geologic Time Scavenger Hunt Name: Class Period: For this activity, go to the resource page on our class website. Find the link titled Understanding Geologic Time which can be found under the Plate Tectonics

More information

GEOLOGY MEDIA SUITE Chapter 8

GEOLOGY MEDIA SUITE Chapter 8 UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 8 Clocks in Rocks Timing the Geologic Record 2010 W.H. Freeman and Company Stratigraphy and fossils Figure 8.4 (page 172)

More information

Petroleum Systems (Part One) Source, Generation, and Migration

Petroleum Systems (Part One) Source, Generation, and Migration Petroleum Systems (Part One) Source, Generation, and Migration GEOL 4233 Class January 2008 Petroleum Systems Elements Source Rock Migration Route Reservoir Rock Seal Rock Trap Processes Generation Migration

More information

These maps make the idea of elevations and contours more tangible follow any of the brown-line contours; they should form a level path.

These maps make the idea of elevations and contours more tangible follow any of the brown-line contours; they should form a level path. Geology 101 Name(s): Lab 1: Maps and geologic time Note: On all labs, you may work in small groups. You may turn in one lab for all of the group members; make sure that everyone who should get credit is

More information

GY 112 Lecture Notes Archean Geology

GY 112 Lecture Notes Archean Geology GY 112 Lecture Notes D. Haywick (2006) 1 GY 112 Lecture Notes Archean Geology Lecture Goals: A) Time frame (the Archean and earlier) B) Rocks and tectonic elements (shield/platform/craton) C) Tectonics

More information

Earth Science 105 Geologic Time Chapter 11

Earth Science 105 Geologic Time Chapter 11 Correlation of rock layers Earth Science 105 Geologic Time Chapter 11 Earth Science 11 th ed. Tarbuck & Lutgens Matching same age rocks In local area Across wide area In different regions Grand Canyon

More information

Earth Science 105. Geologic Time Chapter 11. Earth Science 11 th ed. Tarbuck & Lutgens

Earth Science 105. Geologic Time Chapter 11. Earth Science 11 th ed. Tarbuck & Lutgens Earth Science 105 Geologic Time Chapter 11 Earth Science 11 th ed. Tarbuck & Lutgens Correlation of rock layers Matching same age rocks In local area Across wide area In different regions Grand Canyon

More information

Week 4/5: Limestone & Rock ages

Week 4/5: Limestone & Rock ages Week 4/5: Limestone & Rock ages Monday Warm Up: Write two things you still need to finish in order to be prepared for your presentation tomorrow. LT: I can make a presentation about my solution to a science

More information

Cross-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 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 information

Science 20. Unit C: The Changing Earth. Assignment Booklet C1

Science 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 information

Name HW - Landscapes

Name HW - Landscapes Name HW - Landscapes 1. New York s Tug Hill landscape region is classified as a plateau because this region has a A) high elevation with distorted bedrock B) high elevation with nearly horizontal layers

More information

Name: Date: Period: Page 1

Name: Date: Period: Page 1 Name: Date: Period: Base your answers to questions 1 through 4 on the three bedrock outcrops below and on your knowledge of Earth science. The outcrops, labeled I, II, and III, are located within 15 kilometers

More information

Determining Earth's History Rocks and Ice Cores

Determining 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 information

Absolute Time. Part 8 Geochronology and the Time Scale

Absolute Time. Part 8 Geochronology and the Time Scale Absolute Time Part 8 Geochronology and the Time Scale Unless otherwise noted the artwork and photographs in this slide show are original and by Burt Carter. Permission is granted to use them for non-commercial,

More information

Station Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus

Station 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 information

Fossils and Relative Dating

Fossils and Relative Dating Fossils and Relative Dating OBJECTIVES I can place everyday events in relative order. I can define laws related to the deposition of sediment in water. I can correlate stacks of layered rocks between different

More information

Introduction to Measurements of Physical Quantities

Introduction to Measurements of Physical Quantities 1 Goal Introduction to Measurements of Physical Quantities Content Discussion and Activities PHYS 104L The goal of this week s activities is to provide a foundational understanding regarding measurements

More information

Earth Science. Name Block. Unit 3 Review Worksheet. Circle the letter that corresponds to the correct answer

Earth Science. Name Block. Unit 3 Review Worksheet. Circle the letter that corresponds to the correct answer Earth Science Unit 3 Review Worksheet Name Block Circle the letter that corresponds to the correct answer 1. Which geologic principle is used when a geologist observes an outcrop or rocks and determines

More information

Chapter 3 Time and Geology

Chapter 3 Time and Geology Chapter 3 Time and Geology Methods of Dating Rocks 1. Relative dating - Using fundamental principles of geology (Steno's Laws, Fossil Succession, etc.) to determine the relative ages of rocks (which rocks

More information

NAME: GEL 109 Final Winter 2010

NAME: GEL 109 Final Winter 2010 GEL 109 Final Winter 2010 1. The following stratigraphic sections represents a single event followed by the slow accumulation of background sedimentation of shale. Describe the flows that produced the

More information

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore BEDRO CK For the complete encyclopedic entry with media resources,

More information

Earth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes.

Earth 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 information

Earth s Changing Surface Chapter 4

Earth 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 information

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

8. GEOLOGIC TIME LAST NAME (ALL IN CAPS): FIRST NAME: Instructions LAST NAME (ALL IN CAPS): FIRST NAME: Instructions 8. GEOLOGIC TIME Refer to Exercise 6 in your Lab Manual on pages 151-168 to answer the questions in this work sheet. Your work will be graded on the basis

More information

Tuesday 10 June 2014 Afternoon

Tuesday 10 June 2014 Afternoon Tuesday 10 June 2014 Afternoon A2 GCE GEOLOGY F795/01 Evolution of Life, Earth and Climate *1242977619* Candidates answer on the Question Paper. OCR supplied materials: None Other materials required: Electronic

More information

8(b). Disruption of mats by seismic events

8(b). Disruption of mats by seismic events 1 8(b). Disruption of mats by seismic events J.A. Donaldson and J.R. Chiarenzelli This series of photographs documents structures in quartz arenites of the Nepean Formation (Cambro-Ordovician) in Ottawa,

More information