Fossils and Rock Record

Slides:



Advertisements
Similar presentations
II. Why Do We Study Fossils Found in Rocks?
Advertisements

Earth Science Chapter 21 Section 3
“How can scientists determine the age of rocks and fossils?”
EARTH HISTORY Chapter 6 review.
II. Why Do We Study Fossils Found in Rocks?
Age Dating of Rocks.
Geologic Time Chapter
Geologic Time Who is Stan Hatfield and Ken Pinzke.
Glencoe Earth Science c1999 Chap 12
Prentice Hall EARTH SCIENCE
Ch 8-Rock Record Objectives Principle of uniformitarianism
Rock Record Spring 2013.
Chapter 21 Fossils & the Rock Records
Geologic Time Earth’s History.
Dinosaurs Extinction Theory 12-2
Chapter 17 The Rock Record
DO NOW: Discuss with your table: Where in this picture would you expect to find the OLDEST rocks? Where would you expect to find the NEWEST rocks? What.
UNIT 5: GEOLOGIC HISTORY. AT THE END OF THIS UNIT YOU WILL BE ABLE TO  Calculate the absolute age of a substance based on its decay rate  Correlate.
THIS IS With Host... Your Modified T/F Modified T/F Multiple Choice Multiple Choice Completion.
Geologic Time Chapter 9.
Chapter 12. Warm-up9/1/15  List and briefly describe three different types of fossils.
Define the following terms at the top of your notes for Ch 21!
Chapter 11 Fossils Fossil: evidence such as the remains, imprints, or traces of once living organisms preserved in rocks Many times dead.
THIS IS With Host... Your Relative Dating Absolute Dating Radiometric Dating Fossils Vocabulary 1 Vocabulary 2.
The Rock Record Chapter 8 James Hutton  18 th Century Scottish physician  Observed geologic changes that took place on his farm  By studying the present,
Chapter 8 The Rock Record Chapter 9 The Mesozoic and Cenozoic Eras.
We know Earth is 4.6 Billion years old
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.
Geologic Time The Geologic Time Scale Geologists have divided the history of the Earth in time units based on fossil evidence. The time units are part.
Fossils +/*0 /210.
Mountain Building Folding vs. Faulting Geologic time & dating.
GEOLOGIC TIME & THE EARTH’S HISTORY Part I. The Rock Record  Relative Age  Principle of Uniformitarianism James Hutton 18 th century Scottish physician.
EARTH HISTORY UNIT MS. MITCHELL 9 TH GRADE EARTH SCIENCE VICTORIA MITCHELL 1.
Welcome to Class How do we determine the age of something?
Fossils and the Rock Record
Clues to the Earth’s Past. Paleontology The branch of biology that studies the forms of life that existed in former geologic periods, chiefly by studying.
Chapter 17.1 Principle of Uniformitarianism
I can: describe methods used to assign
Fossils and the Rock Record The Rock Record  Rocks record geological events and changing life forms of the past  Planet Earth was formed 4.6 billion.
Vocab. Fossil Remains, imprints, or traces of prehistoric organisms.
Earth Science With Mr. Thomas. ► Fossils: ► Any evidence of earlier life preserved in rock. ► The study of these fossils is called:
Unit 3 Review Please see pages in your book for more information *This study guide is just to get you started studying– please look at your notes.
The Rock Record Section 3 Section 3: The Fossil Record Preview Objectives Interpreting the Fossil Record Fossilization Types of Fossils Index Fossils Index.
The Fossil Record. 1. Fossils are the remains of organisms that lived in a previous geologic time. 2. The study of these fossils is called paleontology.
Chapter 13 Earth Science Clues to Earth’s Past. Words to Know – Section 1 Fossils fossil Permineralized remains Carbon film Mold Cast Index fossil.
Fossils are the remains, imprints, or traces of prehistoric organisms. Fossils have helped determine approximately when life first appeared, when plants.
The Rock Record Chapter 8 The earth is approximately 4.6 billion years old.
II. Why Do We Study Fossils Found in Rocks? I.What is a Fossil? A. Definition: The evidence or remains of once-living plants or animals A.To provide evidence.
Chapter 16 Fossils and the Rock Record. The Rock Record Geologic Time Scale Divisions of time based on types of fossils found preserved in the rock Present:
How old is old?. Earth Processes take a really, really, really (really) long time….. So, the question is – How do we know how old something is? Especially.
Evidence of a distant past Rocks provide clues to Earth’s past – some of the most obvious clues found in rocks are the remains or traces of ancient living.
Geologic Time. The Geologic Time Scale  A summary of major events in Earth’s past that are preserved in the rock record  Divisions of Geologic Time.
Fossils and the Rock Record
Chapter 8: The Rock Record
Chapter 8 The Rock Record.
II. Why Do We Study Fossils Found in Rocks?
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.
The Rock Record.
Earth History.
Chapter 12 Geologic Time.
Chapter 8-The Rock Record Grand Canyon Video
Earth History.
The fossil record Chapter 8 section 3.
Original Horizontality
Chapter 8 The Rock Record
Fossils Fossil-remains, imprints or traces of prehistoric organisms. Only the hard parts of a plant or animal become fossils. Types of Preservation: --Mineral.
The Geologic Time Scale
Geologic Time Earth Science Ch.12.
Geologic Time Notes By studying the characteristics of rocks and the fossils within them geologists can… interpret the environments in which the rocks.
Chapter 17: Telling Geologic Time
Presentation transcript:

Fossils and Rock Record Chapter 21 Fossils and Rock Record

Vocabulary Uniformitarianism- processes happening today have been happening since Earth formed. (ex. Earthquakes and volcanic eruptions) Relative-age dating- order in which geological event occur. Original horizontality- sedimentary rocks are naturally formed in flat or horizontal layers. Superposition- oldest rock layers are on the bottom and the youngest rock layers are on top.

Vocabulary Cross-Cutting Relationships- intrusions or faults are younger than the layers that they cut across. Principle of Inclusion- inclusions must be older than the rock layer that contain it. Unconformity- a gap in the rock record caused by erosion or weathering. Correlation- matching outcrops of one geographic region to another. Key Bed- a rock or sediment layer used as a marker.

Principles of Determining Relative Age Original Horizontality Superposition Cross-cutting Relationships

Draw a Diagram B A Intrusion Intrusions form when magma is pushed up in between cracks in Earth. Intrusion B A

Create a Diagram Intrusion F Intrusion E D C B A

Questions Rock layers oldest to youngest A, B, C and D- superposition. Intrusion E is younger than layer D, but older than intrusion F- Cross-cutting relationships. Rock layers A,B,C, and D are flat because of original horizontality.

Compare Unconformities Type: disconformity How formed? Sedimentary rock layer deposited on top of an eroded sedimentary rock layer Type: nonconformity How formed? Sedimentary rock layer is deposited on top of an eroded metamorphic or igneous rock layer. Unconformities Type: angular unconformity How formed? Horizontal sedimentary rocks are uplifted and tilted then weather and erode; sedimentary rocks are deposited on top of them, but they are at an angle to the eroded surface.

Other James Hutton and Charles Lyell (Founders of Modern Geology) thought that the “present was the key to the past” – Earth works in an orderly fashion in which natural phenomenon will recur given the same set of conditions.

Vocabulary Drought-extended period of low rainfall. Radioactive Decay- emission of atomic particles Radiometric Dating- process used to determine the absolute age of a rock or fossil by determining the ratio of parent nuclei to daughter nuclei within a given sample. Half-life- period of time it takes a radioactive isotope to decay to ½ of its original amount? Dendochronology- science of comparing annual growth rings in trees to date events and environmental changes. Varve- alternating light-colored and dark-colored sedimentary layers of sand, clay, and silt deposited in a lake that can be used to date cyclic events and changes in the environment. Key Bed- sediment layer that serves as a time marker in the rock record. Similar- nearly the same or alike

Compare absolute and relative dating Relative-Age Dating Ages of rocks and events that formed them in order. Measures The actual age of a rock, fossil, or other object. Absolute-Age Dating

Half-Life Drawing Watch the video clip on half life and draw a simple picture showing what half life is. http://glencoe.com/sec/science/earthscience/2007/concept_motion/animated_art/HalfLife21_15.mpg

Radioactive Decay of Uranium 238 Radioactive Decay of Uranium-238 to Lead-206 Percent Parent Element Daughter Elapsed Years Number of Half-Lives Time 1 100 Time 2 50 4.5 billion 1 Time 3 25 75 9 billion 2 Time 4 12.5 87.5 13.5 billion 3 Time 5 6.25 93.75 18 billion 4

21.4 Vocabulary Trace Fossil- imprints left by organisms that give insight as to how the organisms lived, moved, or obtained food. Index Fossil- the remains of a plant or animal geologists use to correlate or date rock layers.

Useful Fossils Provide information about past environmental conditions Be used to correlate rock layers from one area to another Provide evidence that population have evolved in response to changes in their environments.

Petrification Mineral solutions such as groundwater replace the original organic materials that were covered by layers of sediment with new materials.

Coprolite Fossilized dung or feces from ancient animals.

Gastrulates Dinosaurs had stones in their digestive systems to help digest their food.

Mold and Casts When a shell is buried, its remains decay, and sand or mud fills it in. A cast is a replica of the original organism.

Imprints Carbonized imprints of leaves, stems, flowers, and fish made in soft mud or clay have been found preserved in sedimentary rock.

Freezing The low temperatures of frozen soil and ice can protect and preserve organisms.

Amber Hardened tree sap is called amber. Insects become trapped in the sticky sap and are preserved when the sap hardens.

Mummification Mummified remains are often found in very dry places, because most bacteria which cause decay cannot survive in these places.

What is needed for a index fossil? It must be: It must be distinct abundant widespread existed for only a short span of geologic time. + Write down somewhere on pg. 250

Index Fossils and Relative Age