RF2BD74JR–Fault type vector illustration (3 dimensions) / Left-lateral strike-slip fault
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RF2RT7DP0–Fault type oblique-slip. This photo was taken near Cantavieja, Teruel province, Aragon, Spain.
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RF2BD74PK–Fault type vector illustration (3 dimensions) / Left-lateral strike-slip fault
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RF2BD74PA–Fault type vector illustration (3 dimensions) / Reverse fault
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Heath Road in Twickenham at sunset on an autumn / winter evening when the road is wet and car headlamps light the slippy shiny surface. London. UK. (stockmo) Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/heath-road-in-twickenham-at-sunset-on-an-autumn-winter-evening-when-the-road-is-wet-and-car-headlamps-light-the-slippy-shiny-surface-london-uk-stockmo-image356567366.html
RM2BM318P–Heath Road in Twickenham at sunset on an autumn / winter evening when the road is wet and car headlamps light the slippy shiny surface. London. UK. (stockmo)
Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/triangle-point-is-a-small-promontory-of-overturned-middle-devonian-limestone-intorquay-devon-image474517670.html
RF2JG043J–Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon.
. Bulletin of the Geological Society of America. Geology. SUGGESTIONS FOR TEACHING 183. Figure 13.—Beds repeated at Surface Faults might be introduced in order to make the conception of a fault more accurate and precise. With a more advanced class the local displacements in the different parts of the fault should be described and their characteristics discussed, beginning with a dip-slip fault (the simplest type of fault and fault- movement), all of whose elements can be shown in a vertical section taken at right angles to the strike of the fault and of the strata. With the help of figures 9, Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-geological-society-of-america-geology-suggestions-for-teaching-183-figure-13beds-repeated-at-surface-faults-might-be-introduced-in-order-to-make-the-conception-of-a-fault-more-accurate-and-precise-with-a-more-advanced-class-the-local-displacements-in-the-different-parts-of-the-fault-should-be-described-and-their-characteristics-discussed-beginning-with-a-dip-slip-fault-the-simplest-type-of-fault-and-fault-movement-all-of-whose-elements-can-be-shown-in-a-vertical-section-taken-at-right-angles-to-the-strike-of-the-fault-and-of-the-strata-with-the-help-of-figures-9-image233939985.html
RMRGGTRD–. Bulletin of the Geological Society of America. Geology. SUGGESTIONS FOR TEACHING 183. Figure 13.—Beds repeated at Surface Faults might be introduced in order to make the conception of a fault more accurate and precise. With a more advanced class the local displacements in the different parts of the fault should be described and their characteristics discussed, beginning with a dip-slip fault (the simplest type of fault and fault- movement), all of whose elements can be shown in a vertical section taken at right angles to the strike of the fault and of the strata. With the help of figures 9,
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Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/triangle-point-is-a-small-promontory-of-overturned-middle-devonian-limestone-intorquay-devon-image474518066.html
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. Bulletin of the Geological Society of America. Geology. Figure reverse Fault due to an oolique Slip. determined by the displacement of the stratum, has caused an extension at right angles to the fault strik ». It is evident that if the hanging wall had moved, as in figure 8, with the stratum dipping as there represented, we should have had a normal fault and a contraction at right angles to the fault strike. The relations of the two parts of the disrupted stratum in fig- ure 7 are exactly the same as if we had had a simple reverse dip-slip fault, and in figure 8 as if we had had a simple nor Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-geological-society-of-america-geology-figure-reverse-fault-due-to-an-oolique-slip-determined-by-the-displacement-of-the-stratum-has-caused-an-extension-at-right-angles-to-the-fault-strik-it-is-evident-that-if-the-hanging-wall-had-moved-as-in-figure-8-with-the-stratum-dipping-as-there-represented-we-should-have-had-a-normal-fault-and-a-contraction-at-right-angles-to-the-fault-strike-the-relations-of-the-two-parts-of-the-disrupted-stratum-in-fig-ure-7-are-exactly-the-same-as-if-we-had-had-a-simple-reverse-dip-slip-fault-and-in-figure-8-as-if-we-had-had-a-simple-nor-image233940040.html
RMRGGTWC–. Bulletin of the Geological Society of America. Geology. Figure reverse Fault due to an oolique Slip. determined by the displacement of the stratum, has caused an extension at right angles to the fault strik ». It is evident that if the hanging wall had moved, as in figure 8, with the stratum dipping as there represented, we should have had a normal fault and a contraction at right angles to the fault strike. The relations of the two parts of the disrupted stratum in fig- ure 7 are exactly the same as if we had had a simple reverse dip-slip fault, and in figure 8 as if we had had a simple nor
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RF2CC89MA–Fault type vector illustration (3 dimensions) / Oblique-slip fault
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RF2BD74FT–Fault type vector illustration (3 dimensions) / Right-lateral strike-slip fault
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Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/triangle-point-is-a-small-promontory-of-overturned-middle-devonian-limestone-intorquay-devon-image474517935.html
RF2JG04D3–Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon.
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. Bulletin of the Geological Society of America. Geology. 182 REID ET AL. REPORT ON NOMENCLATURE OF FAULTS ment of the instructor. It would be sufficient to give elementary students a general conception of a fault as a fracture dying out at the ends and. Figure 11.—Section of a normal dip-slip Fault (See figure 9 for legend). Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Geological Society of America. [New York : The Soci Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-geological-society-of-america-geology-182-reid-et-al-report-on-nomenclature-of-faults-ment-of-the-instructor-it-would-be-sufficient-to-give-elementary-students-a-general-conception-of-a-fault-as-a-fracture-dying-out-at-the-ends-and-figure-11section-of-a-normal-dip-slip-fault-see-figure-9-for-legend-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-geological-society-of-america-new-york-the-soci-image233940019.html
RMRGGTTK–. Bulletin of the Geological Society of America. Geology. 182 REID ET AL. REPORT ON NOMENCLATURE OF FAULTS ment of the instructor. It would be sufficient to give elementary students a general conception of a fault as a fracture dying out at the ends and. Figure 11.—Section of a normal dip-slip Fault (See figure 9 for legend). Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Geological Society of America. [New York : The Soci
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RF2BD74PP–Fault type vector illustration (3 dimensions) / Right-lateral strike-slip fault
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Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/triangle-point-is-a-small-promontory-of-overturned-middle-devonian-limestone-intorquay-devon-image474517830.html
RF2JG049A–Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon.
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. Bulletin of the Geological Society of America. Geology. 178 REID ET AL. REPORT OX NOMENCLATURE OF FAULTS. Figure reverse Fault due to an oolique Slip. determined by the displacement of the stratum, has caused an extension at right angles to the fault strik ». It is evident that if the hanging wall had moved, as in figure 8, with the stratum dipping as there represented, we should have had a normal fault and a contraction at right angles to the fault strike. The relations of the two parts of the disrupted stratum in fig- ure 7 are exactly the same as if we had had a simple reverse dip-slip fa Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-geological-society-of-america-geology-178-reid-et-al-report-ox-nomenclature-of-faults-figure-reverse-fault-due-to-an-oolique-slip-determined-by-the-displacement-of-the-stratum-has-caused-an-extension-at-right-angles-to-the-fault-strik-it-is-evident-that-if-the-hanging-wall-had-moved-as-in-figure-8-with-the-stratum-dipping-as-there-represented-we-should-have-had-a-normal-fault-and-a-contraction-at-right-angles-to-the-fault-strike-the-relations-of-the-two-parts-of-the-disrupted-stratum-in-fig-ure-7-are-exactly-the-same-as-if-we-had-had-a-simple-reverse-dip-slip-fa-image233940044.html
RMRGGTWG–. Bulletin of the Geological Society of America. Geology. 178 REID ET AL. REPORT OX NOMENCLATURE OF FAULTS. Figure reverse Fault due to an oolique Slip. determined by the displacement of the stratum, has caused an extension at right angles to the fault strik ». It is evident that if the hanging wall had moved, as in figure 8, with the stratum dipping as there represented, we should have had a normal fault and a contraction at right angles to the fault strike. The relations of the two parts of the disrupted stratum in fig- ure 7 are exactly the same as if we had had a simple reverse dip-slip fa
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Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/triangle-point-is-a-small-promontory-of-overturned-middle-devonian-limestone-intorquay-devon-image474517546.html
RF2JG03Y6–Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon.
. Bulletin of the Geological Society of America. Geology. Figure 13.—Beds repeated at Surface Faults might be introduced in order to make the conception of a fault more accurate and precise. With a more advanced class the local displacements in the different parts of the fault should be described and their characteristics discussed, beginning with a dip-slip fault (the simplest type of fault and fault- movement), all of whose elements can be shown in a vertical section taken at right angles to the strike of the fault and of the strata. With the help of figures 9, 10, 11, and 12, which are sect Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-geological-society-of-america-geology-figure-13beds-repeated-at-surface-faults-might-be-introduced-in-order-to-make-the-conception-of-a-fault-more-accurate-and-precise-with-a-more-advanced-class-the-local-displacements-in-the-different-parts-of-the-fault-should-be-described-and-their-characteristics-discussed-beginning-with-a-dip-slip-fault-the-simplest-type-of-fault-and-fault-movement-all-of-whose-elements-can-be-shown-in-a-vertical-section-taken-at-right-angles-to-the-strike-of-the-fault-and-of-the-strata-with-the-help-of-figures-9-10-11-and-12-which-are-sect-image233939981.html
RMRGGTR9–. Bulletin of the Geological Society of America. Geology. Figure 13.—Beds repeated at Surface Faults might be introduced in order to make the conception of a fault more accurate and precise. With a more advanced class the local displacements in the different parts of the fault should be described and their characteristics discussed, beginning with a dip-slip fault (the simplest type of fault and fault- movement), all of whose elements can be shown in a vertical section taken at right angles to the strike of the fault and of the strata. With the help of figures 9, 10, 11, and 12, which are sect
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Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/triangle-point-is-a-small-promontory-of-overturned-middle-devonian-limestone-intorquay-devon-image474517780.html
RF2JG047G–Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon.
. A bottom gravity survey of the shallow water regions of southern Monterey Bay and its geological interpretation.. Oceanography. A. Inferred CBA Trend (Plan View). N LOW Granite Blocks with Overlying Shale Removed B. Dip-Slip Fault Motion C. Right-Lateral Strike-Slip Fault Motion. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Brooks, Robert Andrew.. Monterey, California: U. S. Naval Postgraduate School Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-bottom-gravity-survey-of-the-shallow-water-regions-of-southern-monterey-bay-and-its-geological-interpretation-oceanography-a-inferred-cba-trend-plan-view-n-low-granite-blocks-with-overlying-shale-removed-b-dip-slip-fault-motion-c-right-lateral-strike-slip-fault-motion-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-brooks-robert-andrew-monterey-california-u-s-naval-postgraduate-school-image234373289.html
RMRH8HEH–. A bottom gravity survey of the shallow water regions of southern Monterey Bay and its geological interpretation.. Oceanography. A. Inferred CBA Trend (Plan View). N LOW Granite Blocks with Overlying Shale Removed B. Dip-Slip Fault Motion C. Right-Lateral Strike-Slip Fault Motion. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Brooks, Robert Andrew.. Monterey, California: U. S. Naval Postgraduate School
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Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/triangle-point-is-a-small-promontory-of-overturned-middle-devonian-limestone-intorquay-devon-image474517464.html
RF2JG03T8–Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon.
. A bottom gravity survey of the shallow water regions of southern Monterey Bay and its geological interpretation.. Oceanography. N LOW Granite Blocks with Overlying Shale Removed B. Dip-Slip Fault Motion C. Right-Lateral Strike-Slip Fault Motion. Figure 19. Two Possible Structural Explanations for the Inferred CBA Field in the Vicinity of the Monterey Submarine Canyon. 77. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Br Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-bottom-gravity-survey-of-the-shallow-water-regions-of-southern-monterey-bay-and-its-geological-interpretation-oceanography-n-low-granite-blocks-with-overlying-shale-removed-b-dip-slip-fault-motion-c-right-lateral-strike-slip-fault-motion-figure-19-two-possible-structural-explanations-for-the-inferred-cba-field-in-the-vicinity-of-the-monterey-submarine-canyon-77-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-br-image234373270.html
RMRH8HDX–. A bottom gravity survey of the shallow water regions of southern Monterey Bay and its geological interpretation.. Oceanography. N LOW Granite Blocks with Overlying Shale Removed B. Dip-Slip Fault Motion C. Right-Lateral Strike-Slip Fault Motion. Figure 19. Two Possible Structural Explanations for the Inferred CBA Field in the Vicinity of the Monterey Submarine Canyon. 77. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Br
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RF2JG0413–Triangle Point is a small promontory of overturned Middle Devonian Limestone inTorquay, Devon.
. Bulletin of the Geological Society of America. Geology. Figure 11.—Section of a normal dip-slip Fault (See figure 9 for legend). Figure 12.—Section of a reverse dip-slip Fault (See figure 9 for legend) varying along its course in the amount, direction, and character (trans- latory or rotatory) of the displacements. The terms defined in the sec- tions on General Terms and General Classes of Local Movements or. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not per Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-geological-society-of-america-geology-figure-11section-of-a-normal-dip-slip-fault-see-figure-9-for-legend-figure-12section-of-a-reverse-dip-slip-fault-see-figure-9-for-legend-varying-along-its-course-in-the-amount-direction-and-character-trans-latory-or-rotatory-of-the-displacements-the-terms-defined-in-the-sec-tions-on-general-terms-and-general-classes-of-local-movements-or-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-per-image233939991.html
RMRGGTRK–. Bulletin of the Geological Society of America. Geology. Figure 11.—Section of a normal dip-slip Fault (See figure 9 for legend). Figure 12.—Section of a reverse dip-slip Fault (See figure 9 for legend) varying along its course in the amount, direction, and character (trans- latory or rotatory) of the displacements. The terms defined in the sec- tions on General Terms and General Classes of Local Movements or. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not per
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