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Page 1: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Page 2: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Page 3: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Page 4: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Page 5: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Page 6: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Page 7: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Page 8: · PDF fileplate movement bend the crust? and observe What happens. ... there is between the opposite sides of the fault. ... Andreas fault, friction is high and the

Note: Chemical Nomenclaturejenfield.rsgc.on.ca/SES4U/Note_Earthquakes.docx · Web viewNote: Earthquakes Elastic Rebound Theory: Earth crust on either side of a fault move in Rather

Name Roy G Biv Dynamic Crust Unit Test - portnet.org · fault motion occurring in Earth’s crust. Which type of fault motion best matches the general pattern of crustal movement

Aim: What are Earthquakes and their characteristics? I. Earthquakes – any vibrating, shaking, or rapid motion of Earth’s crust. A. Fault – zone of weakness

CONTINENTAL CRUST vs. OCEANIC CRUST Solar Wind

Rochester City School District€¦ · Web viewOceanic crust is more dense than continental crust. When oceanic crust and continental crust converge, the more-dense oceanic crust

Ge277-2010 Stress in the crust Implications for fault mechanics and earthquake physics Motivation Basics of Rock Mechanics Observational constraints on

FRACTURES FAULTS FOLDS. Essential QuestionEssential Question How does Elastic Potential Energy cause the Earth’s crust to fracture, fault, and fold?

Crust Mantle Inner Core Outer Core (liquid) · Inner Core (solid) Outer Core (liquid) Mantle Crust . San Andreas Fault . Crust Crust Manu c earth . TEcr0N1c: CYCLE ENERGY nnnn WATER

Dynamic Crust: Earthquakes Final Exam Review. Focus— point beneath the Earth’s surface where fault movement releases seismic waves

Vocabulary Continental Drift Plate tectonics subductiontrench volcanohotspot magmalava convection fault lithosphere mantle crust core

Rocks in the Crust Are Bent, Stretched,...• Fold and Thrust Belts • Fault Block Mountains • Volcanic Mountains Fold and Thrust Mountains 7 Fold and Thrust Mountains Fault Block

Faults & Topography. What’s a Fault? A fault is a break in the rock that makes up the Earth’s crust. The surfaces on either side of the break move past

EARTHQUAKES!!!. Earthquakes Earthquake: Sudden movement of rock sliding along a fault in the earth’s crust Releases energy as this occurs. Energy release

Basin formation by volcanic arc loadingsearg.rhul.ac.uk/pubs/waltham_etal_2008 volcanic arc loading.pdf · Sorong fault zone brought slivers of the continental crust beneath ... volcanic

Earthquakes: vibrations through earth’s crust – Occur when rocks under stress slip or shift along a fault Normally, rocks are pressed together tightly

Menü - Upper Crust · PDF fileMenü - Upper Crust

Earthquakes are the shaking, rolling or sudden shock of the earth’s surface. Earthquakes happen along "fault lines" in the earth’s crust. Earthquakes

Complex fault interaction controls continental rifting€¦ · of deformation through the entire crust and uppermost mantle. Estimates of extension rates during continental rifting18,

Plate Tectonics. Crust The crust is formed from continental and oceanic crust The crust covers the whole Earth

Earthquakes, Volcanoes, and Tsunamis. Earthquakes Fault: a break in the Earths crust. Blocks of the crust slide past each other along fault lines. When

LAB 9: Earthquakes & Seismic Activitystufiles.sanjac.edu/GeneralEducation/2014-2015... · The movement of Earth’s crust along plate boundaries, or fault motion, is the most common

Tectonic implications of fault ... - Macquarie Universityccfs.mq.edu.au/Participants/AI/NDaczkofiles/Pubs/... · tectonic relief for Macquarie Island crust during deposition. Our

Plate Boundaries. Types of Crust Continental Crust Less dense granite Oceanic Crust More dense basalt

Downdip segmentation of strike-slip fault zones in the brittle crust

Move it, move it !!. Fault: a break or fracture in the crust of Earth. Earthquakes: shaking or trembling of the earth caused by movement along a fault

Types of Faults and seismic waves. What is a fault? A fault is a break in the rocks that make up the Earth’s crust, along which rocks on either side have

Seismic Jeopardy!. Seismic Jeopardy! Better Safe than Quarry Hazards!! Locating Quaking Crust in Motion Fault Monitor 10 20 30 40 50

Internal Forces Main Ideas - Weebly · fracture in the earth’s crust is called a fault. It is at the fault line that the plates move past each other. Earthquakes As the plates grind

Earth Science Fall 2013. Earthquake- vibration of the earth’s crust Usually occur when rocks under stress suddenly shift along a fault

Earth Structure. CRUST MANTLE CORE MANTLE CORE CRUST CONTINENTAL CRUST OCEANIC CRUST Peridotite (olivine & augite) Mohorovivic Discontinuity (Moho)

SAN ANDREAS FAULT - CaltechAUTHORSauthors.library.caltech.edu/50925/1/Allen_1957p17.pdf · The San Andreas fault is litera1ly a gigantic fracture in the earth's crust-the principal

Relating Geothermal Resources to Great Basin Tectonics ...geodesy.unr.edu/publications/Blewitt_et_al_GRC05.pdf · fault planes through the entire crust; ... to the Sierran front to

Inner core crust mantle outer core. reverse fault

CONTINENTAL CRUST vs. OCEANIC CRUST

Fault–Block Structure and State of Stress in the Earth’s Crust ...GEOTECTONICS Vol. 43 No. 1 2009 FAULT–BLOCK STRUCTURE AND STATE OF STRESS 69 It is assumed that the rift zone