Impact Craters and Age - Review. Finding ages of objects Absolute ages are assessed through radioactive decay (1/2 lives) – Carbon 14, half-life of 5700.

Slides:



Advertisements
Similar presentations
7.5 Other Objects In the Solar System (Pages ) Homework: Page 306 # 1, 3, 7, 8 Key Concepts: (Page 306)
Advertisements

Who “dun” it? Relative Time: Using layers of sequenced rock to find out which is older and younger Ages of events are placed in order of occurrence.
Who “dun” it? Relative Time: Ages of events are placed in order of occurrence. No exact date is identified. Miss Miller is older than her students. Edison.
Relative Time.
Meteoroids.
What are comets? In 1704 Sir Edmond Halley hypothesized that the comets of 1456, 1532, 1607, 1682 were the same object. He calculated a 75.7 year orbit.
Age Dating Rocks.
Impacts with Space Objects. Moon shows many impact scars though most are prior to 3.8 billion years ago.
Remnants of Rock and Ice Asteroids Meteoroids (meteorites, meteor) Comets.
Absolute Dating : A Measure of Time
Absolute vs. Relative Dating of Rocks
OTHER OBJECTS IN THE SOLAR SYSTEM
Take up worksheets -other objects in solar system -solar system chart.
Goal:  I will be able to explain what relative and absolute age are and how we determine them.  I will be able to explain the Law of Superposition, including.
Absolute Dating Chapter 7 Lesson 2.
How can scientists determine the ages of fossils and rocks?
What Processes Shape our Earth?.  Geology: the scientific study of the origin, history, structure, and composition of the Earth  Importance: Understanding.
Volcanoes, Earthquakes, Tsunamis What do you know? What are some things you want to learn or questions you have?
Impacts of Meteors Meteor: Glowing fragments from outside the atmosphere that burn upon entry Meteorite: Piece of rock that strikes earth from space Asteroid:
Unit 7 Lesson 3 Absolute Dating
EARTH ORIGIN S. * 78.0% 43.0% 9.3% 8.0% 0.1% 3.8% % of Earth’s History P.
Asteroids, Meteors, and Comets. What are they? How are they different from each other?
7.2 Half-Life the time it takes for half of a radioactive sample to decay is a constant rate (always the same half life for each element) Example: Strontium-90.
History of Life: Origins of Life Chapter Age of Earth The earth is about 4.5 billion years old How did we measure that? Radiometric Dating = calculating.
Other Celestial Objects Comets, Asteroids, Meteoroids, Meteors, and Meteorites.
Comets, Asteroids, Meteoroid and Meteorites Chapter 21 Section 5 Pages
Meteors. Ground Zero What is the chance of being near (within 1 km) a meteor as it strikes the ground during your lifetime? A. About 1 in a thousand.
Interplanetary Bodies. Asteroids Solid bodies having no atmosphere Have well determined orbits More than 2000 in our solar system.
Geologic Time. What is Geology? Geology is the study of the Earth’s form and composition and the changes it has undergone.
Small Bodies in the Solar System
Half- Life. Some minerals contain radioactive elements. Some minerals contain radioactive elements. The rate at which these elements decay (turn into.
Ch. 23.6: Interpreting the Rock Record
Absolute vs. Relative Dating
Impacts on Earth. Read The Crater That Ended the Reign of the Dinosaurs. Answer the questions in your journal. How big would this crater be in Phoenix?
Giant Impacts Impacts long ago in the Solar System? Recent impacts? Likelihood of a life- threatening impact with Earth? What would happen? What happens.
IT CAME FROM Asteroids, comets, and YOU. Formation of the Solar System.
Cratering in the Solar System Lab 8. Properties of Craters Craters formed by asteroids and comets able to penetrate the planet’s atmosphere An impactor.
Impact What is the chance of being near (within 1 km) a meteor as it strikes the ground during your lifetime? A. About 1 in a thousand. B. About the same.
Tips on Dating. Why Date? Different methods of dating will help determine the actual age of a layer of rock or a fossil Scientists look at how much radioactive.
Section 2: Determining Absolute Age
Mountain Building Folding vs. Faulting Geologic time & dating.
Warm-up 1. How do scientists use ‘relative dating?’ 2. Which layer is the oldest? 3. Which layer is the youngest? 4. Which layers are older than the fault.
Radioactive Dating Chapter 7 Section 3.
Chapter 7.2 – Half life Science 10. Types of decay Alpha Alpha.
Chapter 8 The Moon. Orbital Properties Distance between Earth and Moon has been measured to accuracy of a 3 cm using lasers Distance of the moon from.
Announcements Homework: Chapter 8 # 46, 47, 50 & 51 plus Estimate the size of the meteor that formed Barringer’s Crater in Arizona. Assume it was a pure.
Unit 2 Lesson 3 Absolute Dating Copyright © Houghton Mifflin Harcourt Publishing Company.
Methods of Measurement
1 Earth’ s History Unit 6. 2 Vocabulary List 1.Relative Dating 2.Absolute Dating 3.Superposition 4.Cross-cutting relationships 5.Uniformitarianism 6.Original.
Vagabonds of the Solar System Lecture 27. Main-belt asteroids 2.0 – 3.5 AUs.
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.
2/25/20161 Geologic Time Mr. Litaker. Objectives  State the principle of uniformitarianism.  Explain how the law of superposition can be used to determine.
Geologic Time MMSA Earth-Space Science. -Time scale based upon the fossil record -The fossil record indicates a wide variety of life has existed on Earth.
The Rock Record Section 2 Section 2: Determining Absolute Age Preview Objectives Absolute Dating Methods Radiometric Dating Radioactive Decay and Half-Life.
Other Solar System Bodies next right hand side Key Point (8-4.1): Summarize the characteristics and movements of objects in the solar system.
Absolute Dating: A Measure of Time January 27,2015.
Geological Time Dating Absolute and Relative. Geologic Time B y examining layers of sedimentary rock, geologists developed a time scale for dividing up.
Impact craters are geologic structures formed when a large meteoroid, asteroid or comet smashes into a planet or a satellite.Impact craters are geologic.
Chapter 23 Solar System Section 3 Asteroids, Comets and Meteoroids Notes 23-5.
Geological Time Dating Absolute and Relative. Geologic Time B y examining layers of sedimentary rock, geologists developed a time scale for dividing up.
Absolute Dating.
ABSOLUTE AGE DATING Absolute Age Dating is finding the numerical age of an object Artifacts (rocks or fossils) contain radioactive elements which are.
Science 7: Unit E: Planet Earth Topic 9 – Geologic Time.
Applications. The half-life of a radioactive substance is the time it takes for half of the atoms of the substance to become disintegrated. All life on.
The Solar System Pt. 2 Bolides & Behaviors (29.4)
Impacts on Earth Barringer (Meteor) Crater, Arizona 50,000 years old.
CRATER INVESTIGATION.
Asteroids, Meteors & Comets, Oh My!
Comets, Asteroids and Meteors
Presentation transcript:

Impact Craters and Age - Review

Finding ages of objects Absolute ages are assessed through radioactive decay (1/2 lives) – Carbon 14, half-life of 5700 years – Uranium 238, half-life of 700 million years! Requires lab analysis of physical samples

How it works Each half life reduces the amount of the radioactive element by 1/2 – 2 half lives = 1/4 the amount left – 3 half lives = 1/8 the amount left If a half life is 700 million years, and there is 1/8 the original amount left… – 1/8 amount = 3 half-lives x 700 million years = ??? – 2100 million (2.1 billion) years.

No lab samples, no problem! Craters can provide a RELATIVE age – Formation of craters (and other features) will not always happen in a fresh area. – They overlap each other!

Crosscutting and Superposition Older craters/features are broken up and overlaid by newer features – Superposition: craters overlapping others – Crosscutting: features sliced through by channels Try it again:

Try again A B C

Crater Classification Erosion of a crater can happen *anywhere* – (it is just faster on some astronomical bodies that others…) – The appearance of a crater can reveal its (relative) age – 3 main classes Preserved (A) Modified (B) Destroyed (C)

Describe the main feature - HYPOTHESIZE!

Which is the older surface? How do you know?

A second method Crater Density Method! It’s pretty simple: – More craters = older! This assumes relatively stable rates of impacts over time. Also, assumes relatively even distribution.

Famous impacts Many on earth, but hard to see sometimes… Not always though!

Barringer Crater Arizona, 50,000 years ago 1.2 km diameter, 0.2 km deep Created by 300,000 ton iron meteor, 50 m 20 km/s

Tunguska Event 1908, Siberia – Blue column of light – Bright as the sun! Object airburst – Broke apart before hitting the ground Blast = 1000x hiroshima – Knocked down 80 million trees over 2,150 km 2 – Blew out windows several hundred km away

Peekskill Meteorite 1992, Eastern US 12 kilo stony meteor First major meteor captured on video from multiple angles/areas Recovered and sold for $70,000

Chicxulub! Dino Killer! PDX sized object! 200 km crater! Global effects!

k-t

Shoemaker-Levy fragments Each left an impact scar the size of earth.