PDF-, A. C., B Deformation of the Continental Crust: The 272

572J L MUNTEAN Fig1 Shaded relief map of north. 2 Complete all information requested on the online form available at wwwcontinentaltirepromotionsca or this mail in form accurately and legibly and SURYLGH57347D57347FRS57347RI57347RXU57347UHWDLOHU57526V573475HFHLSW57347WKDW57347FOHDUO57347LQGLFD te Continental Crust. Chapter 10. Hypsographic Curve. Continental Crust Terms. Orogeny. Epeirogeny. Terrane. Accreted Terrane. Mantle Plume. Hot Spot Volcanism. Wilson Cycle. Basin . Dome. Accretion. Craton. Notes. Geology – . the study of the Earth and its processes. 2. The Earth’s. . Layers. Scientists study seismic (earthquake) waves and volcanic explosions to learn about the Earth’s interior.. Isostasy. When . gravitational and buoyant forces are equal, a state of . isostasy. exists. . As . erosion wears away the crust, the lithosphere becomes lighter and rises. .. As . erosion continues, the . Selwyn’s career goal #__: What does the . asthenosphere. have to do with earthquakes, crustal motions, and mantle convection?. Upper crust. Lower crust. Upper mantle. Upper crust. Lower crust. Upper mantle. Part I: Dynamic Earth. The Northern Lights / Aurora borealis. Created. . in. . part. . from. . the. . electro. . magnetic. . field. . from. . the. . earth’s. . core. New Area of Focus: Earth’s Plate Boundaries.. Lower Crust . and . Upper Mantle: Evidence . from . Rock Mechanics, Geodesy, and . Field Observations. Roland . Burgmann. . and Georg . Dresen. Key Purposes. Concerned . with describing material properties through constitutive equations that relate . How Rocks Deform. Deformation. . . = bending, tilting, or breaking Earth’s crust.. Isostasy. Deformation can be due to two opposing forces:. gravity, or weight, of the . lithosphere. pressing down on the . Kinematic analysis of deformation. B. Natalin. Stress, strain, and deformation. The . stress . (σ) acting on a plane is the force per unit area of the plane (σ = . F. /area).. The. deformation . refers to changes in shape, position, or orientation of a body resulting from the application of a differential stress (i.e., a state in which the magnitude of stress is not the same in all directions).. M. Zollhöfer, E. Sert, G. Greiner and J. Süßmuth. Computer Graphics Group, University Erlangen-Nuremberg, Germany. Motivation/Requirements. Intuitive modeling. Handle-based. Direct manipulation. 2. No major . tectonism. , . magmatism. , basement metamorphism or . anorogenic. intrusion since . t. he Cretaceous. No rifting, major extension or . transtension. since the . Paleogene. Schulte and Mooney (2005). Lesson. . Objectives:. To understand what occurs at different plate boundaries.. Success Criteria:. Create an annotated diagram of each plate boundary.. Plate 1. Plate 2. Continental crust. THE WORLD’S MAIN PLATE BOUNDARIES. No major . tectonism. , . magmatism. , basement metamorphism or . anorogenic. intrusion since . t. he Cretaceous. No rifting, major extension or . transtension. since the . Paleogene. Schulte and Mooney (2005). The thin brittle shell is the crust that humans live on.. The thick jelly like white is the deep hot magma beneath the surface.. The yellow yolk is the core of the earth.. Tectonic Map of the World. A tectonic plate is like the hard shell on a boiled egg that has been cracked into .