Lab 1: Stress, Mohr`s circles SOLUTION KEY
... Range) plate boundaries. The minimum principal stress is oriented vertically for convergent boundaries and thrust faults; horizontally for divergent boundaries and normal faults. We expect that both maximum and minimum princi pal stresses are horizontal for transform boundaries or strikeslip fault ...
... Range) plate boundaries. The minimum principal stress is oriented vertically for convergent boundaries and thrust faults; horizontally for divergent boundaries and normal faults. We expect that both maximum and minimum princi pal stresses are horizontal for transform boundaries or strikeslip fault ...
normal fault - Madison County Schools
... rocks break, slip apart, or change shape. Shearing happens when two plates slip past each other in opposite directions. ...
... rocks break, slip apart, or change shape. Shearing happens when two plates slip past each other in opposite directions. ...
Earthquakes/Mountain Building
... • The movement causes stress in the crust. • There are 3 types of stress in the crust • Stress -pressure ...
... • The movement causes stress in the crust. • There are 3 types of stress in the crust • Stress -pressure ...
PowerPoint
... its shape & volume • Adds energy to rock until it breaks or changes shape • Causes deformation • Rocks can break…creating a fault • Causes earthquakes ...
... its shape & volume • Adds energy to rock until it breaks or changes shape • Causes deformation • Rocks can break…creating a fault • Causes earthquakes ...
Forces in the Crust Day 2 - Hicksville Public Schools / Homepage
... AIM: Describe the types of stress and the land features (faults,uplift,folds) that result from forces (stress) in the Earth’s crust? OBJ: Given notes and activity sheet SWBAT describe the types of stress and the land features (faults, uplift, folds) that result from forces (stress) in the Earth’s cr ...
... AIM: Describe the types of stress and the land features (faults,uplift,folds) that result from forces (stress) in the Earth’s crust? OBJ: Given notes and activity sheet SWBAT describe the types of stress and the land features (faults, uplift, folds) that result from forces (stress) in the Earth’s cr ...
Grain Size Determination
... Other defects exist in all solid materials that are much larger than those heretofore discussed. These include pores, cracks, foreign inclusions, and other phases. They are normally introduced during processing and fabrication steps. Grain Size Determination The grain size is often determined when t ...
... Other defects exist in all solid materials that are much larger than those heretofore discussed. These include pores, cracks, foreign inclusions, and other phases. They are normally introduced during processing and fabrication steps. Grain Size Determination The grain size is often determined when t ...
Lecture22_deformation
... Faults The actual atomic bonds within the rock are broken along the zone of max stress = where the crack appears Occurs under conditions of low temp and pressure Also occurs when stress is applied quickly, a quick swing of a hammer ...
... Faults The actual atomic bonds within the rock are broken along the zone of max stress = where the crack appears Occurs under conditions of low temp and pressure Also occurs when stress is applied quickly, a quick swing of a hammer ...
EarthquakefaultsPowerpointnew
... caused by the abrupt release of stress…which has built up over a long time. ...
... caused by the abrupt release of stress…which has built up over a long time. ...
Deformation of the Crust
... – Distorts rock by pushing parts of the rock in opposite directions. – Rocks bend, twist, or break as they slide past each other. – Common at transform boundaries ...
... – Distorts rock by pushing parts of the rock in opposite directions. – Rocks bend, twist, or break as they slide past each other. – Common at transform boundaries ...
Folds and Faults - hrsbstaff.ednet.ns.ca
... Compression – occurs at converging plates; rocks generally thicken and shorten Tension – occurs at diverging plates; rocks generally thin and lengthen Shearing – occurs at transform plate boundaries; rocks are sliced into parallel blocks ...
... Compression – occurs at converging plates; rocks generally thicken and shorten Tension – occurs at diverging plates; rocks generally thin and lengthen Shearing – occurs at transform plate boundaries; rocks are sliced into parallel blocks ...
Page 1
... 10. Shaking and trembling that results from the movement of rock beneath Earth’s surface Shearing directions ...
... 10. Shaking and trembling that results from the movement of rock beneath Earth’s surface Shearing directions ...
ppt - Discover Earth Science
... • INCLUDED FRAGMENTS: pieces of rock found IN another rock must be OLDER (formed first). ...
... • INCLUDED FRAGMENTS: pieces of rock found IN another rock must be OLDER (formed first). ...
Section: Deforming the Earth`s Crust
... ______ 7. The bending of rock layers due to stress is known as a. faulting. c. divergence. b. folding. d. convergence. Match the correct definition with the correct term. Write the letter in the space provided. a. anticline b. monocline c. syncline ...
... ______ 7. The bending of rock layers due to stress is known as a. faulting. c. divergence. b. folding. d. convergence. Match the correct definition with the correct term. Write the letter in the space provided. a. anticline b. monocline c. syncline ...
the present-day tectonic stress pattern of australia
... orientation of the SHmax at the basin, field and well scale. The new ASM database suggests a thrust faulting stress regime typically exists in the upper one km of the crust. This regime changes to a prevailing strike-slip faulting stress regime in deeper parts. A comparison between the Australian ne ...
... orientation of the SHmax at the basin, field and well scale. The new ASM database suggests a thrust faulting stress regime typically exists in the upper one km of the crust. This regime changes to a prevailing strike-slip faulting stress regime in deeper parts. A comparison between the Australian ne ...
Jeopardy - Effingham County Schools
... To support his hypothesis, Wegener provided evidence from ……, traces of ancient organisms preserved in rock ...
... To support his hypothesis, Wegener provided evidence from ……, traces of ancient organisms preserved in rock ...
Slides for lecture #23
... Small time dependent effects can be observed also for elastic deformation - e.g. related to reversible diffusion of C in a steel under stress. If a sample is vibrated close to resonance, the deviation from perfect elasticity, i.e. the existence of dissipative processes, results in a change of the re ...
... Small time dependent effects can be observed also for elastic deformation - e.g. related to reversible diffusion of C in a steel under stress. If a sample is vibrated close to resonance, the deviation from perfect elasticity, i.e. the existence of dissipative processes, results in a change of the re ...
Geologic Structure Part I – Folds
... Folds Anticline Tension Faults Break Plastic deformation h) Syncline i) Brittle deformation j) Force/stress ...
... Folds Anticline Tension Faults Break Plastic deformation h) Syncline i) Brittle deformation j) Force/stress ...
19.1 Earthquakes Power point
... Woodville. The photo is looking northeast. The lateral or strike-slip fault offset is large; however, the trace is nearly invisible. This earthquake, together with the fire that followed, resulted in more than 3,000 deaths and 400 million dollars of property damage. [Photo credit: G.K. Gilbert, U.S. ...
... Woodville. The photo is looking northeast. The lateral or strike-slip fault offset is large; however, the trace is nearly invisible. This earthquake, together with the fire that followed, resulted in more than 3,000 deaths and 400 million dollars of property damage. [Photo credit: G.K. Gilbert, U.S. ...
Geology of the Hawaiian Islands
... shape or size that is not recovered when the stress is removed • Occurs by the slippage of atoms or small groups of atoms past each other in the deforming material, without loss of cohesion ...
... shape or size that is not recovered when the stress is removed • Occurs by the slippage of atoms or small groups of atoms past each other in the deforming material, without loss of cohesion ...