'Normal faults' diaporamas de présentation

Table of Contents

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Chapter 4 Lesson 1: Forces In Earth's Crust 1. How Does Stress Change Earth's Crust?

Chapter 4 Lesson 1: Forces In Earth's Crust 1. How Does Stress Change Earth's Crust? 2. How Do Faults Form 3. How Does Plate Movement Create New Landforms?. Stress & Change > The Earth's crust is sorta like a candy bar. ------> What the heck do I mean? . 1.

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Folding and Faulting

Folding and Faulting. Chapter 4, Sec. 4. Stress. Amount of force per area put on an object. Rocks can change shape due to stress. Three types of stress:. Compression Tension Shear. FOLDING. Rock layers bend due to stress Assume most rocks are laid down horizontal. FAULTS.

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Seismic Reflection Data: what it is, how it can be used, & an application at Elk Hills, CA

Seismic Reflection Data: what it is, how it can be used, & an application at Elk Hills, CA. - Hudec and Martin, 2004. Seismic Reflection Data: Definition. Seismic Reflection. return of a wave from a surface that it strikes into the medium through which it has traveled.

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Earthquakes

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Earthquakes

Amanda Embrey and Steven Bomar Chapter 8. Earthquakes. Even though we believe that earthquakes are just ground tremors, they are way more complex than that. In order to understand them more, we use seismology (the study of earthquakes). What are earthquakes?.

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Guadalupe Mountains

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Fault and folding

Earth 238-23. Fault and folding. *Fault-bend folds. Earth 238-23. Fault and folding. Earth 238-23. Fault and folding. Earth 238-23. Fault and folding. Earth 238-23. Fault and folding. *Fault-bend folds develop in normal fault systems, most notably rollover anticlines. Earth 238-23.

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F 3 - Faults, Fractures and Flexures in Three-Dimensions:

F 3 - Faults, Fractures and Flexures in Three-Dimensions: Field Observations at the Dead Sea Basin Ze'ev Reches School of Geology and Geophysics, University of Oklahoma. Multi-scale deformation in basin margins: A. Bending of the crust into the basin B. Zig-zag faulting in basin margins

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Earthquakes

Earthquakes. Pages B104-B127. Faults are classified by how rocks move. The blocks of rock along different types of faults move in different directions, depending on the kinds of stress they are under. There are three types of faults: Normal Faults Reverse Faults Strike-Slip Faults.

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Some Thoughts on IMW And Opportunity

Some Thoughts on IMW And Opportunity. We represent a big area of the ANSS national program. Bob Smith Univ. of Utah. What We Are Up Against! $4.1B US, with only $0.2B in the Intermountain West. FEMA Annualized Earthquake Loss Estimate (2000).

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Evidence about Past Earthquakes From Faults

Evidence about Past Earthquakes From Faults. By: Thomas Solowynsky, Tom Mulally, Victoria Flis, Omar Oregel . Faults. There are many faults that tell us different effects and are caused by earthquakes. Faults form because of extension or compression.

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Types of Mountains: Folded Mountains. Pressure is applied slowly to the

Types of Mountains: Folded Mountains. Pressure is applied slowly to the rock so that it bends instead of breaking. Makes folds in the rocks. Faulted Mountains. Pressure breaks the land, causing land to move up r down. Resulting in higher areas (mountains).

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Formation of the American Southwest (including Nevada)

Formation of the American Southwest (including Nevada). Basin and Range Geology . Hundreds of Millions of Years Ago The American Southwest was under water . Sediment piled creating layers of Sedimentary Rock . The Land was uplifted creating a flat plateau . Plateau: very Flat land.

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Rates of Plates

Rates of Plates . Reflect & Connect #1-5 p. 670-672.

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Tectonics of the Eastern Great Basin

Tectonics of the Eastern Great Basin. Tyler Szwarc and Mark Gorenc. The Great Salt Lake Basin. Bounded by normal faults that reach up down to 5 km into the crust. Cenozoic sediments fill the grabens up to 10,000 feet.

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Types of Faults

Types of Faults. Strike Slip Fault: Two layers of rock are shifted horizontally or parallel to the fault plane. . 1) "Hanging Wall "- The surface of block that is ontop of the plane of the fault. 2) "Footwall" - The surface or block that lies below the plane of the fault.

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Name: Matthew Moore Organization: Western Oregon University Email: MatthewTMs@Gmail

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Assessment of CO 2 Storage and Migration in the Nugget Sandstone, Moxa Arch, Wyoming

(core data). (B). (core data). Assessment of CO 2 Storage and Migration in the Nugget Sandstone, Moxa Arch, Wyoming. Shuiquan Li, lishuiquan@tsinghua.org.cn ; Ye Zhang, yzhang9@uwyo.edu. Geological Modeling & Simulation Group.

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