Stratigraphy DEFINITION OF STRATIGRAPHY DEFINITION OF STRATIGRAPHY 1. Branch of geology that deals with definition & description of major & minor natural.

Slides:



Advertisements
Similar presentations
Summer School Geosciences Geology Lecture 2 Stratigraphy.
Advertisements

An Introduction To Sedimentology And Stratigraphy
Time and Geology Sir Charles Lyell Image source:
Unit 6 – The Geosphere Vocabulary
Earth and Space Sciences Unit 4
EARTH SYSTEMS Daily plans. 1/28/15 EQ: How does the study of our atmosphere impact our understanding of geological time? Reminder: Test makeup Opening:
Earth History GEOL 2110 Lecture 7 Fundamentals of Stratigraphy I
Stratigraphy and fossils
Stratigraphy Rocks, Fossils, and Time.
Introduction to stratigraphy Establishing relationships between rocks.
Time and Geology. The Present is the Key to the Past –Catastrophism-October 23, :00AM James Ussher, Bishop of Ireland –Uniformitarianism- James.
HOW OLD IS OLD? The Rock Record and Geologic Time Chapter 3
CEE 437 Lecture 1 October 1, 2002 Thomas Doe. Outline Course Introduction Geology and Engineers Brief History of Geology Global Structure Plate Tectonics.
Historical Geology Introduction. What is Historical Geology? Earth’s History based on evidence preserved in rocks Immensity of time span difficult to.
What’s so remarkable about Hutton’s Ideas?
GEOLOGIC PRINCIPLES & RELATIVE DATING. HOW OLD IS THE EARTH? The Earth is about 4.6 billion years old Much of its history is recorded in the rocks Observations.
Greeks and Romans Recognized world was ever changing and thought of it as eternal Fall of Rome and Rise of Church Developed idea of world based on a literal.
Geology. The study of the solid Earth and the processes that shape it – Plate tectonics – Past climates – Natural disasters – Fossil Record – Evolution.
1 Chapter 1 Earth System History. 2 Study of the inter- connected physicochemical and biological changes that our planet has experienced over the course.
CLOCKS IN ROCKS Timing the Geologic Record. The Stratigraphic Record Important Principles 1.Original horizontality—sediments were deposited originally.
VISUALIZING EARTH HISTORY
HISTORICAL GEOLOGY LECTURE 1. STRATIGRAPHY Stratigraphy:
WELCOME TO CLASS. Agenda TODAY Sequencing Time Rock Record Notes Relative Age activity Hand back tests NEXT TIME Absolute age lab Geologic Time QUIZ.
What Processes Shape our Earth?.  Geology: the scientific study of the origin, history, structure, and composition of the Earth  Importance: Understanding.
Discovering Earth’s History Rocks Record Earth’s History 1. Rocks record geological events and changing life forms of the past. 2.Scientists have learned.
Interpreting Earth’s Rocks to Determine Its Past History.
Ch.6 Earth’s History. Who’s got the TIME? RELATIVE: order/sequence known, but not the actual date of occurrence. “Time Line” ABSOLUTE: actual date determined.
Relative Age Dating Uniformitarianism Principles of correlation
Geologic Time. Super what??!?!  Superposition: Younger rock layers are on top of older rock layers.  Used with the other principles of stratigraphy.
Time and Geology Sir Charles Lyell Image source:
Geological Time Geology 12. Uniformitarianism “The present is the key to the past”- the fundamental principle that underlies most of geology. Put simply,
21.2 – Relative Age Dating How can you tell if one rock layer is older than another? How can you tell if one fossil is older than another? What is an index.
Earth History GEOL 2110 Midterm 1 Preparation/Review.
Scientific Dating Methods Unit 5. Scientific dating methods of fossils and rock sequences are used to construct a chronology of Earth’s history expressed.
Stratigraphy Stratigraphy is the branch of geology that deals with the arrangement of rocks in layers.
The fossil of one of the earliest birds, called archaeopteryx, shows reptile-like features. It lived during the late Jurassic period, about 105 my ago.
Principles of Historical Geology III Historical Geology – Principles III.
Lecture 2 Introduction to Earth History. IComponents of Geology A)Physical Geology B)Historical Geology IIFounders of A)James Ussher B)Nicolaus Steno.
A Little Bit of History … The history of geologic time begins with the human interest in mining. Interests in rock units began to flourish with commercial.
A Little Bit of History… The history of geologic time begins with the human interest in mining. Interests in rock units began to flourish with commercial.
GEOLOGICAL TIME. GEOLOGY NEEDS A TIME SCALE An investigation of the history of Earth Understanding how features of landscape developed and formed Reconstructing.
STRUCTURAL GEOLOGY  PRIMARY & NON-TECTONIC STRUCTURES 1) PRINCIPLE OF ORIGINAL HORIZONTALITY (NICOLAS STENO ) – LAYERS OF SEDIMENTS ARE ORIGINALLY.
Earth’s History How do we know about it?. What is Uniformitarianism? Uniformitarianism: –Is a theory developed by the Scottish geologist, James Hutton,
Geologist interpret Earth’s history by studying sedimentary rocks Relative Dating.
Geology 101 David Brown. James Hutton ( CE) Scottish geologist Scottish geologist Developed the laws of geology Developed the laws of geology.
Interpreting Ancient Environments
Visualizing Earth Science By Z. Merali and B. F. Skinner Chapter 10 – How Old is Old? The Rock Record and Deep Time.
Relative dating methods and the time divisions of Earth history Geology 103.
Introduction A. Beginning- (~1500AD) da Vinci saw fossils in rks of Italian Apennines Concluded fossils once living marine organisms Concluded fossils.
History of the Discipline: Geology & Paleontgology
MSc. Paleontology and Stratigraphy
Earth History Dating geologic events like volcanic eruptions, uplift, subsidence, deposition, impacts, intrusion, ice ages, etc.
The Fundamental Laws of Geology Several principles or “laws” are fundamental to the geologic interpretation of a sequence of events.
HOW OLD IS OLD? The Rock Record and Deep Geologic Times.
21.2 – Relative Age Dating. Interpreting Geology James Hutton, a Scottish geologist who lived in the late 1700s Attempted to explain Earth ’ s history.
Tahsin Islam University of Barisal.. Stratigraphy: Stratigraphy is the study of rock layers (strata) and their relationship with each other. Stratigraphy.
Time and History of Earth
Seismic, Sequence and Magnetic Stratigraphy
What are Fossils? Fossils are the evidence or remains of once-living plants or animals Fossils provide evidence of past existence of a wide variety of.
Geologic Time Uniformitarianism vs. Catastrophism.
Earth systems Daily plans.
Time and Stratigraphy Basics
Thank you for not chewing gum 
Harry Williams, Historical Geology
How Old is Old? Geologic Time.
Determining Relative Age
EARTH AND SPACE SCIENCE
TIME.
Igneous Intrusion Fault. Igneous Intrusion Fault.
The Rock Record.
Presentation transcript:

Stratigraphy DEFINITION OF STRATIGRAPHY DEFINITION OF STRATIGRAPHY 1. Branch of geology that deals with definition & description of major & minor natural division of rocks... w/ the interpretation of their significance in geologic history. 1. Branch of geology that deals with definition & description of major & minor natural division of rocks... w/ the interpretation of their significance in geologic history. 2. Specifically, the geologic study of the form, arrangement, geographic distribution, chronological succession, classification & esp. correlation and mutual relationships of rock strata in normal sequence. 2. Specifically, the geologic study of the form, arrangement, geographic distribution, chronological succession, classification & esp. correlation and mutual relationships of rock strata in normal sequence. 3. It involves interpretation of these features of rock strata in terms of origin, occurrence, environment, thickness, lithology, composition, fossil content, age, history, paleogeography etc 3. It involves interpretation of these features of rock strata in terms of origin, occurrence, environment, thickness, lithology, composition, fossil content, age, history, paleogeography etc

Introduction A. Beginning- (~1500AD) da Vinci saw fossils in rks of Italian Apennines Concluded fossils once living marine organisms Concluded fossils once living marine organisms

Introduction B. Steno important contributor Principle of Original Horizontality Principle of Original Horizontality Principle of Superposition Principle of Superposition Principle of Lateral Continuity Principle of Lateral Continuity

Steno Principles Lateral Continuity Superposition Original Horizontality

Development of Sed Strat as Science Organization of sed rocks—Arduino ( ) divided rocks Organization of sed rocks—Arduino ( ) divided rocks Primary Mtns- metallic ores no fossils Primary Mtns- metallic ores no fossils Secondary Mtns- Stratified, lithified, fossiliferous, no fossils Secondary Mtns- Stratified, lithified, fossiliferous, no fossils Tertiary low Mtns- Fossiliferous, unconsolidated gravels, sands clay, volcanics Tertiary low Mtns- Fossiliferous, unconsolidated gravels, sands clay, volcanics Alluvium- Sediment washed down from mtns Alluvium- Sediment washed down from mtns

Development of Sed Strat as Science Geologic Cycle and Uniformitarianism Geologic Cycle and Uniformitarianism James Hutton ( )-Scottish Physician, farmer James Hutton ( )-Scottish Physician, farmer  Noted cyclicity to earth’s behavior  Uplift, erosion, transport, deposition  Established Principle of Uniformitarianism or Actualism present key to past but rates change and catastrophes occur present key to past but rates change and catastrophes occur

Development of Sed Strat as Science – Birth of Biostratigraphy & Stratigraphic Correlation William Smith( )-English surveyor, engineer  “father” of biostratigraphy  Canal builder noted relationship of fossils & rocks  Established law of faunal succession—fossils succeed each other in organized & recognizable fashion  Produced first geologic map gsahist.org

Birth of Biostratigraphy & Stratigraphic Correlation  D’Orbigny (1842)- developed biologic stage for rock division  strata systematically follow each other with characteristic fossil assemblage  Oppel (1856)- developed biologic zone  Rocks deposited during existence of specific fossil  Zones based of first appearance of last appearance of organisms  Zones could be correlated

Oppel Zones

Development of Sed Strat as Science Petrographic microscope development Petrographic microscope development Sorby began microscopic study of rocks Sorby began microscopic study of rocks Led to description and systematic study of rocks Led to description and systematic study of rocks Geologic Revolution- Seafloor Spreading and Plate Tectonics Geologic Revolution- Seafloor Spreading and Plate Tectonics s- Renaissance period s- Renaissance period More funds, more geophysical exploration, Deep Sea Drilling Project More funds, more geophysical exploration, Deep Sea Drilling Project More oil exploration More oil exploration

New Tools New Tools Magnetic and Seismic Surveying Magnetic and Seismic Surveying Identification of normal/reverse periods led to magnetostratigraphy Identification of normal/reverse periods led to magnetostratigraphy Seismic surveying could identify units and unconformities, packages of related rocks Seismic surveying could identify units and unconformities, packages of related rocks Isotope stratigraphy Isotope stratigraphy Use carbon and oxygen isotopes to correlate units Use carbon and oxygen isotopes to correlate units petroleum-gas.blogspot.com

Magnetostratigraphy sp.lyellcollection.org

Seismic Stratigraphy www-odp.tamu.edu

Development of Sed Strat as Science Sedimentary Rocks and Earth History Sedimentary Rocks and Earth History Paleoclimate Paleoclimate study of ancient climate study of ancient climate

Development of Sed Strat as Science Sedimentary Rocks and Earth History Sedimentary Rocks and Earth History Paleogeography Paleogeography reconstruction of area for given time in past reconstruction of area for given time in past Wiley.com

Development of Sed Strat as Science Sedimentary Rocks and Earth History Sedimentary Rocks and Earth History Paleoecology & Evolution Paleoecology & Evolution studies relationships between ancient organisms & their environments studies relationships between ancient organisms & their environments jpg

Development of Sed Strat as Science Sedimentary Rocks and Earth History Sedimentary Rocks and Earth History Paleoceanography & Ancient Atmosphere Paleoceanography & Ancient Atmosphere Composition of ancient oceans and atmosphere using isotopes Composition of ancient oceans and atmosphere using isotopes