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Figure 4.24 Transform faults and fracture zones along an oceanic ridge. Transform faults are fractures along which lithospheric plates slide horizontally past one Plate boundary Oceanic ridge another. Transform faults are Adjacent sections here move in same Sections here Adjacent sections here move in same the active part of fracture zones. For a review of this move in opposite direction directions direction process in larger scale, please see Figure 3.25. Fracture Transform fault Fracture (active part of fracture zone) zone zone (inactive) (inactive) Lithosphere Asthenosphere Transform faults (orange) form because the axis of Alaska seafloor spreading on the surface of a sphere cannot follow a smoothly curving Aleutian Trench line. The motion of two di- verging lithospheric plates (arrows) rotates about an imaginary axis extending through Earth. Queen Charlotte Fault Canada Juan de Fuca- Ridge Cascadian Subduction Zone Mendocino Fracture Zone NORTH AMERICAN PLÄTE San Andreas Fault Gulf of California Mexico PACIFIC PLATE Rivera Fault East Pacific Rise сосos PLATE b A long transform plate boundary, which indludes California's San Andreas Fault. Note the offset plate boundaries caused by divergence on a sphere. California's San Andreas Fault, a transform fault. The fault trace is clearly visible between the arrows in this photograph taken south of San Francisco. The fault takes its name from San Andreas Lake, visible near the center of the photograph. The large landfill is the site of San Francisco International Airport. Figure 3.25 Transform faults. Tom Gar ison Buj weejebebuego O Cengaga Learning

Figure 4.24 Transform faults and fracture zones along an oceanic ridge. Transform faults are fractures along which lithospheric plates slide horizontally past one Plate boundary Oceanic ridge another. Transform faults are Adjacent sections here move in same Sections here Adjacent sections here move in same the active part of fracture zones. For a review of this move in opposite direction directions direction process in larger scale, please see Figure 3.25. Fracture Transform fault Fracture (active part of fracture zone) zone zone (inactive) (inactive) Lithosphere Asthenosphere Transform faults (orange) form because the axis of Alaska seafloor spreading on the surface of a sphere cannot follow a smoothly curving Aleutian Trench line. The motion of two di- verging lithospheric plates (arrows) rotates about an imaginary axis extending through Earth. Queen Charlotte Fault Canada Juan de Fuca- Ridge Cascadian Subduction Zone Mendocino Fracture Zone NORTH AMERICAN PLÄTE San Andreas Fault Gulf of California Mexico PACIFIC PLATE Rivera Fault East Pacific Rise сосos PLATE b A long transform plate boundary, which indludes California's San Andreas Fault. Note the offset plate boundaries caused by divergence on a sphere. California's San Andreas Fault, a transform fault. The fault trace is clearly visible between the arrows in this photograph taken south of San Francisco. The fault takes its name from San Andreas Lake, visible near the center of the photograph. The large landfill is the site of San Francisco International Airport. Figure 3.25 Transform faults. Tom Gar ison Buj weejebebuego O Cengaga Learning

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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How is California’s famous San Andreas Fault related to transform faults and
fracture zones?

Figure 4.24 Transform faults and fracture zones along an oceanic ridge. Transform faults are fractures along which lithospheric plates slide horizontally past one Plate boundary Oceanic ridge another. Transform faults are Adjacent sections here move in same Sections here Adjacent sections here move in same the active part of fracture zones. For a review of this move in opposite direction directions direction process in larger scale, please see Figure 3.25. Fracture Transform fault Fracture (active part of fracture zone) zone zone (inactive) (inactive) Lithosphere Asthenosphere
Transcribed Image Text:Figure 4.24 Transform faults and fracture zones along an oceanic ridge. Transform faults are fractures along which lithospheric plates slide horizontally past one Plate boundary Oceanic ridge another. Transform faults are Adjacent sections here move in same Sections here Adjacent sections here move in same the active part of fracture zones. For a review of this move in opposite direction directions direction process in larger scale, please see Figure 3.25. Fracture Transform fault Fracture (active part of fracture zone) zone zone (inactive) (inactive) Lithosphere Asthenosphere
Transform faults (orange) form because the axis of Alaska seafloor spreading on the surface of a sphere cannot follow a smoothly curving Aleutian Trench line. The motion of two di- verging lithospheric plates (arrows) rotates about an imaginary axis extending through Earth. Queen Charlotte Fault Canada Juan de Fuca- Ridge Cascadian Subduction Zone Mendocino Fracture Zone NORTH AMERICAN PLÄTE San Andreas Fault Gulf of California Mexico PACIFIC PLATE Rivera Fault East Pacific Rise сосos PLATE b A long transform plate boundary, which indludes California's San Andreas Fault. Note the offset plate boundaries caused by divergence on a sphere. California's San Andreas Fault, a transform fault. The fault trace is clearly visible between the arrows in this photograph taken south of San Francisco. The fault takes its name from San Andreas Lake, visible near the center of the photograph. The large landfill is the site of San Francisco International Airport. Figure 3.25 Transform faults. Tom Gar ison Buj weejebebuego O Cengaga Learning
Transcribed Image Text:Transform faults (orange) form because the axis of Alaska seafloor spreading on the surface of a sphere cannot follow a smoothly curving Aleutian Trench line. The motion of two di- verging lithospheric plates (arrows) rotates about an imaginary axis extending through Earth. Queen Charlotte Fault Canada Juan de Fuca- Ridge Cascadian Subduction Zone Mendocino Fracture Zone NORTH AMERICAN PLÄTE San Andreas Fault Gulf of California Mexico PACIFIC PLATE Rivera Fault East Pacific Rise сосos PLATE b A long transform plate boundary, which indludes California's San Andreas Fault. Note the offset plate boundaries caused by divergence on a sphere. California's San Andreas Fault, a transform fault. The fault trace is clearly visible between the arrows in this photograph taken south of San Francisco. The fault takes its name from San Andreas Lake, visible near the center of the photograph. The large landfill is the site of San Francisco International Airport. Figure 3.25 Transform faults. Tom Gar ison Buj weejebebuego O Cengaga Learning
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