logging in or signing up lec 2 09 Felipe Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 278 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: November 05, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Today – 2/9: Today – 2/9 Weather report Review The magnetic field and the sea floor! Workshop Review session: Mon 5-7, Chavez 110Last Time: Last Time Continental drift rejected despite good evidence because no mechanism conceivable Seismic profiling reveals internal structure of the Earth Convecting outer core powers geodynamo, creating Earth’s magnetic fieldEarth’s Magnetic Field: Earth’s Magnetic Field Diverts solar wind, which would destroy ozone layer and ruin electronics Guides migrating animals from bacteria to bees to sea birds to toothed whalesEarth’s Magnetic Field: Earth’s Magnetic Field Reverses it polarity occasionally! Interacts with solar storms to produce the aurora borealis Leaves its signature in magnetic rocks like magnetite“Halloween” Solar Storm: “Halloween” Solar Storm www.nasa.govSolar Storm: Solar Storm www.nasa.govAurora from Space: Aurora from Space www.nasa.govMagnetism in Minerals: Magnetism in Minerals Each electron has “spin”, i.e. acts as a tiny bar magnet Electrons pair up in orbitals around nuclei; the electrons in a pair have opposite polarity Lone electrons in an orbital impart a net magnetic moment to an atom If the magnetic atoms in a mineral are all oriented identically, the mineral is magneticMagnetite: Magnetite The crystal structure of magnetite allows magnetic iron atoms to retain their magnetic orientation Above “Curie point”, 580 °C, atoms too energetic to be permanently magnetized Below Curie point, atoms line up with Earth’s magnetic field, the mineral becomes permanently magnetized and records the orientation of Earth’s magnetic field at the time the magnetite cooled through the Curie point Early 1900’s scientists recognized that magnetism in Earth’s rocks comes in two flavors: same polarity as today or oppositeOld Assumptions re Ocean Floor: Old Assumptions re Ocean Floor 4 Ga Flat and featureless Deeply buried in sedimentMid-Ocean Ridges (MORs): Mid-Ocean Ridges (MORs) Naval survey, mid-1800’s Sonar developed 1906 for icebergs, adapted for submarine detection WWI Mid-ocean ridges: giant mountain chains running down the center of the oceans After WWII, Atlantic sea floor sediment found to be a thin veneerMagnetic Striping of the Sea Floor: Magnetic Striping of the Sea Floor Magnetometers developed WWII for submarine detection Used to explore the magnetic properties of the sea floor during the 1950’s Magnetic striping: found alternating bands of reversed magnetic polarity in the rocks running parallel to the MOR’s! Pattern symmetrical about the MOR’s!Sea Floor Spreading!: Sea Floor Spreading! 1968 – Glomar Challenger drills the ocean floor across the S Atlantic from S America to Africa Retrieved rocks show that ages decrease to zero at the MAR, then increase, so new oceanic crust is being created at the MAR! The core has revealed to us the mechanism for continental drift!Age of the Atlantic Sea Floor: Age of the Atlantic Sea Floor www.noaa.govAge of the Sea Floor: Age of the Sea Floor www.pubs.usgs.govSlide16: pubs.usgs.govWorkshop: Workshop Distance = rate time, d = rt t = d/r r = d/t Rate of sea floor spreading = 2 distance from rock to ridge / age of rockExample: Example 90 km atlas.geo.cornell.eduBack in the Lab: Back in the Lab Isotopic analysis reveals that the rock is 3 Ma What is the rate of sea floor spreading? Clear Unclear: Clear Unclear You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
lec 2 09 Felipe Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 278 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: November 05, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Today – 2/9: Today – 2/9 Weather report Review The magnetic field and the sea floor! Workshop Review session: Mon 5-7, Chavez 110Last Time: Last Time Continental drift rejected despite good evidence because no mechanism conceivable Seismic profiling reveals internal structure of the Earth Convecting outer core powers geodynamo, creating Earth’s magnetic fieldEarth’s Magnetic Field: Earth’s Magnetic Field Diverts solar wind, which would destroy ozone layer and ruin electronics Guides migrating animals from bacteria to bees to sea birds to toothed whalesEarth’s Magnetic Field: Earth’s Magnetic Field Reverses it polarity occasionally! Interacts with solar storms to produce the aurora borealis Leaves its signature in magnetic rocks like magnetite“Halloween” Solar Storm: “Halloween” Solar Storm www.nasa.govSolar Storm: Solar Storm www.nasa.govAurora from Space: Aurora from Space www.nasa.govMagnetism in Minerals: Magnetism in Minerals Each electron has “spin”, i.e. acts as a tiny bar magnet Electrons pair up in orbitals around nuclei; the electrons in a pair have opposite polarity Lone electrons in an orbital impart a net magnetic moment to an atom If the magnetic atoms in a mineral are all oriented identically, the mineral is magneticMagnetite: Magnetite The crystal structure of magnetite allows magnetic iron atoms to retain their magnetic orientation Above “Curie point”, 580 °C, atoms too energetic to be permanently magnetized Below Curie point, atoms line up with Earth’s magnetic field, the mineral becomes permanently magnetized and records the orientation of Earth’s magnetic field at the time the magnetite cooled through the Curie point Early 1900’s scientists recognized that magnetism in Earth’s rocks comes in two flavors: same polarity as today or oppositeOld Assumptions re Ocean Floor: Old Assumptions re Ocean Floor 4 Ga Flat and featureless Deeply buried in sedimentMid-Ocean Ridges (MORs): Mid-Ocean Ridges (MORs) Naval survey, mid-1800’s Sonar developed 1906 for icebergs, adapted for submarine detection WWI Mid-ocean ridges: giant mountain chains running down the center of the oceans After WWII, Atlantic sea floor sediment found to be a thin veneerMagnetic Striping of the Sea Floor: Magnetic Striping of the Sea Floor Magnetometers developed WWII for submarine detection Used to explore the magnetic properties of the sea floor during the 1950’s Magnetic striping: found alternating bands of reversed magnetic polarity in the rocks running parallel to the MOR’s! Pattern symmetrical about the MOR’s!Sea Floor Spreading!: Sea Floor Spreading! 1968 – Glomar Challenger drills the ocean floor across the S Atlantic from S America to Africa Retrieved rocks show that ages decrease to zero at the MAR, then increase, so new oceanic crust is being created at the MAR! The core has revealed to us the mechanism for continental drift!Age of the Atlantic Sea Floor: Age of the Atlantic Sea Floor www.noaa.govAge of the Sea Floor: Age of the Sea Floor www.pubs.usgs.govSlide16: pubs.usgs.govWorkshop: Workshop Distance = rate time, d = rt t = d/r r = d/t Rate of sea floor spreading = 2 distance from rock to ridge / age of rockExample: Example 90 km atlas.geo.cornell.eduBack in the Lab: Back in the Lab Isotopic analysis reveals that the rock is 3 Ma What is the rate of sea floor spreading? Clear Unclear: Clear Unclear