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pompously    
ad. 傲慢地;豪华地;壮观地

傲慢地;豪华地;壮观地


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  • Fault Models - Carleton College
    Fault models aid in visualizing and understanding faulting and plate motions because the educator and their learners can manipulate a 3-D model for a true hands-on experience These models represent Earth faulting and plate tectonic structures and motions
  • 3 Types of Faults: Normal, Reverse and Strike-Slip - Earth How
    All plate tectonic boundaries are faults because they always have movement relative to each other By definition, plate tectonics always converge, diverge, or slide across each other NORMAL: Normal faults occur at divergent plate boundaries REVERSE: Reverse faults are at convergent plates
  • Geologic Structures – Historical Geology
    Normal Faults A normal fault is caused by extensional (tensional) stress at divergent plate boundaries as two plates are moving in opposite directions, away from each other In a normal fault, the hanging wall has moved down relative to the footwall
  • Chapter 10: Deformation and Structures – Investigating the Earth . . .
    Normal faults are common in divergent tectonic settings, whereas thrust and reverse faults are common in convergent tectonic settings Horizontal motion is called strike-slip or transform; these are common in transform plate boundaries
  • Activity— Foam Faults - Cascadia Earthscope Earthquake and Tsunami . . .
    Demonstrate plate tectonic principles, plate boundary interactions and the geometry and relative motions of faulting of geologic layers using 3-D foam models
  • 22—PLATE-TECTONIC FEATURES - USGS
    Active transform fault, left-lateral offset—Approxim-ately located Arrows show relative motion Active transform fault, normal offset—Approximately located Hachures on downthrown side Ancient convergent plate boundary—Approximately located Sawteeth on upper plate Active convergent plate boundary—Accurately located Sawteeth on upper plate
  • Activity modified from L. W. Braile, Purdue University
    This is called “normal faulting” when the block above a fault moves down with respect to the block below the fault The down-dropped block is called a “graben”
  • 13. 3 Fractures, Joints, and Faults - University of Saskatchewan
    Tension produces normal faults, in which the crust undergoes extension This permits the hanging wall to slide down the footwall in response to gravity (Figure 13 25, left)
  • Teaching About Plate Tectonics and Faulting Using Foam Models
    Objective: Demonstrate plate tectonic principles, plate boundary interactions and the geometry and relative motions of faulting of geologic layers using 3-D foam models
  • Year 11 Earth and Environmental Science Depth Study Module 2
    plate tectonics at each plate boundary type? Students: Model types of plate boundaries showing the dominant topographic and geological features, including: (ACSES006) • divergent boundaries: rift valley, mid-ocean ridge, normal and transform faults, • convergent boundaries: mountain range, trench, reverse faults and folds





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