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Plate Tectonics Overview. What are plates?. Rigid, moving sections of the lithosphere (land) that float on the A sthenosphere. Major tectonic process. There are three main tectonic process Folding Faulting V ulcanism. Folding.
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What are plates? • Rigid, moving sections of the lithosphere (land) that float on the Asthenosphere
Major tectonic process • There are three main tectonic process • Folding • Faulting • Vulcanism
Folding • When rock layers compress under great stress they form folds. • Easily seen where roads have been made into hillsides.
Faulting • Four types of faults • Normal: upward movement of one side of the fault line • Reverse: when one block moves upwards against another • Strike-Slip: where two sections of rock move horizontally past each other • Fault Scarps: created by normal or reverse faulting using in a straights or continuous line across landscape for a considerable amount of distance
Vulcanism • Associated with violent volcanic actvity. • Caused by convergent and subduction zones.
Types of Plate boundaries • Three main types: • Diverging • Transform fault • Converging
Plate movement and they results • Diverging: volcanic or faulting process • Transform fault: faulting process (earthquake) • Converging: folding, faulting, and volcanic processes • Violent and destructive
Other Plate Tectonic Facts • Plate interiors are relatively free from tectonic activities (are not impacted)
Other plate tectonic facts • The world’s continents were once part of a supercontinent, which broke up 200 million years ago.