3/6/021 Impact features Meteor Crater near Flagstaff, AZ.

Slides:



Advertisements
Similar presentations
Relative Dating of Rocks
Advertisements

Earth Science 12.1 Discovering Earth’s History: Geologic Time
Meteors And Meteorites
Asteroids, Meteors and Meteoroids Asteroids Name meaning “star-like bodies” AKA “minor planets” or “planetoids” Move along a very eccentric path Mostly.
Impact. The Solar System Nine Eight Planets Over 100,000 catalogued asteroids ???? Centaurs ???? KBO’s (including one disgruntled ex- planet) Millions.
LEQ: How do geologists and paleontologists determine the relative age of rocks? Part 1 Key Terms: Absolute Age, Relative Age, Law of Superposition,
Meteoroids.
1. Location: 35.4N, 111.5W Elevation: 8,026 feet (2,447 m) Sunset Crater is in the eastern part of the San Francisco volcanic field. Sunset Crater is.
Lunar Crater Lab. What is a Crater? Round depressions in the surface Caused by a meteorite hitting the surface.
Craters of the Moon Read Ch. 4 of the text, sections 4.1 through 4.6.
Welcome Students!.
25.1 ORIGIN AND PROPERTIES OF THE MOON DAHS MR. SWEET
By Stephen Monahan. Discovered by Luis and his son Walter Alvarez in 1980 Proposed Asteroid Theory.
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.
Travel-time versus Distance Curves
Basic Structure of the Earth
Just about everyone wanted to know about the circles on the Moon. In the 1960’s two distinguished geologists thought about the craters on the surface.
Meteors - Matter that falls through Earth’s atmosphere. Often called “shooting stars”. A few can be observed every hour.
Section 1: Earth’s Moon Preview Key Ideas Exploring the Moon
Collisions in the solar system Collisions have played a major part in both the formation and the evolution of the solar system Q: Can you give a number.
P1 The Earth in the Universe IP1.10 Lesson Objectives To revise our knowledge of the solar system To explain the impact of asteroids and comets.
1 Daily Warm-Up Exercises Day 46 In the Grand Canyon, there is a layer of Coconino Sandstone directly above a layer of Hermit Shale. Which layer is older?
I. The Highlands  Surface feature that is light in color, high in elevation (mountainous), and heavily cratered.
Quick Write: Geologists have devised methods to estimate the ages of rocks in the Grand Canyon. Geologists have determined: The Earth is probably 4.5 billion.
Small Bodies in the Solar System
Impact Craters Meteorites & Asteroids
Earth And Moon. The name of Earth’s moon is Luna. Imagine that you have just landed on Luna’s surface. What do you imagine the surface of our moon is.
Impact Craters.
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.
06/08/03 COMETS AND IMPACT CRATORS Mullard Space Science Laboratory University College London
Moon Impact Studies. What do We Know About the Moon?
The Grand Canyon Megan Pickard TESSE Law of Original Horizontality Sediments are deposited in layers that are horizontal.
LEQ: How do geologists and paleontologists determine the relative age of rocks? Part 1 Key Terms: Absolute Age, Relative Age, Law of Superposition, 1.
The Rock Record Section 1 Section 1: Determining Relative Age Preview Objectives Uniformitarianism Relative Age Law of Superposition Principle of Original.
Earth’s Moon Section Surface of the Moon Maria – dark, flat areas of rock formed from lava flows Galileo thought they were oceans.
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.
Tuesday December 7, 2010 (Review for Test 5). The Launch Pad Tuesday, 12/7/10 No Launch Pad Today.
Sponge – What is a synchronous orbit?. Surface Features - Maria - oceans or seas. (Galileo thought they were oceans when he saw them through his.
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.
Mars Student Imaging Program The Three Principles Impact Craters Features you must know and understand. Ejecta – Material, from the crater, that was thrown.
Planetary image interpretation and mapping Phil Stooke USGS map I-515.
Meteor seen Over Des Moines, Iowa. The Loenid Meteor Shower.
Galileo Galilei Looking through one of his telescopes, Galileo observed the dark spots on the moon. As the moon revolved, the darkness shifted and new.
Bradley Central High School
The Rock Record Section 1 Section 1: Determining Relative Age Preview Objectives Uniformitarianism Relative Age Law of Superposition Principle of Original.
The Solar System 1 _________________ 9 _________________ planets ________ (major) moons asteroids, comets, meteoroids.
Impact craters are geologic structures formed when a large meteoroid, asteroid or comet smashes into a planet or a satellite.Impact craters are geologic.
Don’t Waste Time! Chapter 6: The Rock and Fossil Record.
Planets. The terrestrial planets and some large moons.
Chapter 4 The Solar System.
The Asteroid Belt and Beyond!
Impact Craters Meteorites & Asteroids
Meteors and Meteorites
Impact Craters Jagmark
NOTES: Behaviors & Bolides (29.4)
The Sun, Earth and Moon.
TASK H Compare the image of the Earth showing the location of known impact sites (red dots on map) and compare it with the image of the Moon. Although.
Section 1: Earth’s Moon Preview Key Ideas Exploring the Moon
Section 1: Earth’s Moon Preview Key Ideas Exploring the Moon
Deeper, and Deeper, and Deeper
Relative Dating.
The Solar System Pt. 2 Bolides & Behaviors (29.4)
Impacts on Earth Barringer (Meteor) Crater, Arizona 50,000 years old.
History of Life on Earth
Asteroids, Meteors & Comets, Oh My!
Sponge – What is a synchronous orbit?
Section 1: Earth’s Moon.
COMETS, ASTEROIDS, METERORS, AND METEROIDS!
Plate tectonics on Earth
Presentation transcript:

3/6/021 Impact features Meteor Crater near Flagstaff, AZ

3/6/022 Instructor has no financial or other interest in Meteor Crater. It’s just a neat place to see.

3/6/023 Characteristics Bowl-shaped raised rim (~100 feet) diameter ~4000 feet depth ~600 feet fragments of an iron meteorite in vicinity (Canyon Diablo meteorite) 25, ,000 years old volcanoes nearby (5 million years old)

3/6/024 Meteor Crater, Arizona

3/6/025 History 1876 Mathias Armijo, cowboy –visited by prospectors, metal fragments –thought to be volcanic 1891 sample of metal sent for analysis –77% iron –2% lead –rest gold and silver

3/6/ A E Foote, a mineralogist, visits –identifies metal fragments as a meteorite –diamonds found in meteorite –crater due to impact 1895 G K Gilbert, Director USGS –not an impact –volcanic 1902 D M Barringer, mining engineer –graduated Princeton at 19 –law school

3/6/027 –studied geology at Harvard –wanted to work in west –discovered Commonwealth silver mine, AZ –rich –visited crater site, was of meteorite origin –bought the place! 1906 published paper outlining his ideas B convinced that a large (several million tons) iron meteorite buried below the crater, worth ~$250,000,000

3/6/028 Barringer’s arguments in favor of impact origin –surrounded by millions of tons of debris pulverized sandstone (Coconino) –oxidized chunks of iron –meteorite fragments mixed with rock debris –overturned rim –no volcanic rocks in crater –no magnetic effect - iron in small pieces

3/6/029 Detailed history and info. –gdcinfo.agg.nrcan.gc.ca:80/crater/ –index_e.html

3/6/0210 Gilbert’s arguments in favor of volcanic origin –no evidence of a large meteorite –no magnetic effect from meteorite –not necessary to have lava in the crater –crater the result of high pressure steam

3/6/0211 Test: A. volcanic - no magnetic effect; volumes equal B. impact - should be a magnetic effect, unequal volumes Gilbert measured and A was correct

3/6/0212 Barringer Drilling in center - nothing decided that the meteorite buried beneath south rim 1919 Gilbert reiterates volcanic theory 1920 B raises more money; drill sticks and breaks - meteorite? 1925 mine shaft - floods, company sinks, B dies

3/6/0213 Geology Couldn’t be simpler (layer cake) horizontal layers of sedimentary rocks each of a different color only three rocks involved –lowest is the Coconino sandstone (white) –middle is the Kaibab limestone (buff) –uppermost is the Moenkopi sandstone (purple)

3/6/0214 Layer-cake arrangement of sedimentary rocks youngest on top excavation rim deformation of the rocks

3/6/0215 New player Eugene Shoemaker PhD from Princeton University doctoral dissertation, Meteor Crater idea that a high velocity object hitting the Earth would be largely vaporized old idea now the ability to simulate with computer

3/6/0216 Mid 1960s

3/6/0217 Estimates Iron meteorite 100 feet in diameter 63,000 tons 15 km/sec energy ~120 megatons of TNT greater than the nuclear device dropped on Hiroshima

3/6/0218 High velocity; example Buffalo - New York is 450 miles =730 km at 15 km/sec, the trip would take 49 seconds meteorites can have velocities of 70 km/sec trip to NY would take 10 seconds And you would be driving a car that weighed 63,000 tons (don’t hit anything!)

3/6/0219 In spite of that - Meteor Crater is a small event.

3/6/0220 Underground nuclear test: Project Sedan

3/6/0221 Overturned rim; reversal of rocks

3/6/0222 Overturned rim: oldest rock on top

3/6/0223 Crater types: bowl shaped, small raised rim Meteor Crater central peak larger terraces Copernicus

3/6/0224 Isidorus, Moon

3/6/0225 Theophilus, Moon

3/6/0226 Gosses Bluff, Australia