plate tectonics chapters 7, 8, & 9 test 2 material end

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PLATE TECTONICS Chapters 7, 8, & 9 Test 2 material End

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  • Slide 1
  • Slide 2
  • PLATE TECTONICS Chapters 7, 8, & 9 Test 2 material End
  • Slide 3
  • LEGEND AZTEC INDIANS OF MEXICO SACRIFICED HUMANS TO KEEP AWAY EARTHQUAKES AND TO KEEP SUN ALIVE BY CUTTING OUT THE HEARTS OF THEIR VICTIMS AND THROWING THEM INTO VOLCANO
  • Slide 4
  • LEGEND IN WESTERN AFRICA THOUGHT THE JUNGLE WAS THE HAIR OF A GIANT. ALL LIVING THINGS THAT CREPT OR CRAWLED IN THE JUNGLE WERE LIKE LICE IN THE GIANTS HAIR. EARTHQUAKES WERE EXPLAINED AS THE GIANT SHAKING HIS HEAD TO GET RID OF THE LICE
  • Slide 5
  • LEGEND IN POLYNESIA TWO GODDESSES WERE FIGHTING THEIR WAY ACROSS THE PACIFIC. WHEREVER AN EARTHQUAKE OR VOLCANO OCCURRED, THIS WAS A BATTLE SITE. WHEN A GODDESS WAS SPURNED BY A LOVER SHE THREW A TANTRUM AND LAVA FLOWED
  • Slide 6
  • LEGEND VULCAN WAS THE ROMAN GOD WHO HAD A FORGE AT THE CENTER OF THE EARTH TO MAKE WEAPONS FOR THE GODS. WHENEVER HIS FORGE WAS WORKING LAVA SPEWED FORTH AT THE SURFACE.
  • Slide 7
  • LEGEND IN ICELAND VIKING LEGEND TALKS OF ODIN & FRIGGA AND THEIR BELOVED SON BALDER. THE GOD OF MISCHIEF, LOKI, CONSPIRED TO HAVE BALDER KILLED.
  • Slide 8
  • FAMOUS VOLCANOES IN HISTORY MOUNT VESUVIUS MOUNT PELEE - WITH GLOWING CLOUD (NUEE ARDENTE) PARICUTIN KRAKATOA
  • Slide 9
  • VESUVIUS
  • Slide 10
  • MT PELEE
  • Slide 11
  • PARICUTIN
  • Slide 12
  • Volcanoes Birth of Paricutin
  • Slide 13
  • FAMOUS EARTHQUAKES GREAT ALASKA QUAKE OF 1964 GREAT CHINA QUAKE NEW MADRID QUAKES OF 1811-1812 MISSISSIPPI RIVER STOOD UP ON END CHURCH BELLS RANG IN BOSTON http://www.youtube.com/watch?v=4Y- 62Ti5_6s http://www.youtube.com/watch?v=4Y- 62Ti5_6s Pakistan quake of 2006
  • Slide 14
  • DR. IBEN BROWNING 1990 PREDICTED A 50% CHANCE OF EARTHQUAKE OF 6.5 - 7.5 IN NEW MADRID BETWEEN DEC. 1-5, 1990 CLAIMED A GREAT TIDAL STRAIN WOULD ALSO STRAIN THE SUBSURFACE RECEIVED NOTORIETY FOR PREDICTING SF QUAKE OF 1989
  • Slide 15
  • ARGUMENTS AGAINST DR. BROWNINGS THEORY NO FIRM SCIENTIFIC SUPPORT FOR HIS THEORY WAS A BIOLOGIST SPECIALIZING IN CLIMATOLOGY AND WAS NOT A GEOLOGIST OR SEISMOLOGIST ERRONOUS CLAIM TO FAME FOR PREDICTING SAN FRANCISCO EARTHQUAKE OF 1989
  • Slide 16
  • TRANSCRIPTS REVEALED BROWNING PREDICTED AN EARTHQUAKE OF 6.0+ WOULD OCCUR SOMETIME ON OR AROUND OCT 16TH (ACTUAL QUAKE WAS 17TH) SOMEWHERE IN WORLD. THESE QUAKES HAPPEN EVERY 3 DAYS SO NOT MUCH OF A FORECAST
  • Slide 17
  • THE ONLY GEOLOGIST IN THE NATION SUPPORTING HIM HAD SHAKEY REPUTATION. HAD FLOWN OVER THE STATE OF NORTH CAROLINA USING A PSYCHIC TRYING TO LOCATE AREAS WHERE AN EARTHQUAKE WOULD STRIKE
  • Slide 18
  • Slide 19
  • ALFRED WEGENER THEORY OF CONTINENTAL DRIFT & PLATE TECTONICS PANGAEA LAURASIA GONDWANA GLOSSOPTERIS
  • Slide 20
  • Slide 21
  • WHAT WAS EFFECT OF CONTINENTAL MOVEMENT? NEW CLIMATES ALONG COASTS NEW MOUNTAIN RANGES NEW DESERTS DRIFTING OF THE POLES PLANT AND ANIMAL LIFE SIMILARITIES IN AREAS ONCE UNITED
  • Slide 22
  • Slide 23
  • Slide 24
  • SEA FLOOR SPREADING WEGENERS HYPOTHESIS WAS NOT READILY ACCEPTED BECAUSE IT FAILED TO PROVIDE MECHANISM FOR MOVEMENT ARTHUR HOLMES, GEOLOGIST THOUGHT THE SEA FLOORS WERE DRAGGING ALONG THE CONTINENTS WHICH RESTED ON TOP OF THEM
  • Slide 25
  • Seafloor spreading
  • Slide 26
  • THOUGHT CONVECTION PROCESS BEGAN BELOW EARTHS SURFACE WHICH PUSHED MATERIAL UPWARD TO FORM RIDGE SYSTEMS ON OCEAN FLOOR. MATERIAL WIDENS THE OCEANS BY 1 OR 2 INCHES PER YEAR
  • Slide 27
  • WHAT DID HOLMES FIND ON OCEANIC RIDGES? EQUAL DISTANCE EQUAL AGE EQUAL THICKNESS EQUAL MAGNETIC DIRECTION WHAT DOES THIS SUGGEST?
  • Slide 28
  • PLATE BOUNDARIES DIVERGENT CONVERGENT TRANSFORM
  • Slide 29
  • DIVERGENT PLATE BOUNDARIES FOUND NEAR SPREADING CENTERS & AT THE MID-OCEANIC RIDGE SYSTEMS RIFT VALLEYS GREAT RIFT VALLEY OF AFRICA
  • Slide 30
  • divergent
  • Slide 31
  • Rift valley
  • Slide 32
  • East africa rift
  • Slide 33
  • CONVERGENT PLATE BOUNDARIES OCEAN & CONTINENT OCEAN & OCEAN CONTINENT & CONTINENT
  • Slide 34
  • convergent
  • Slide 35
  • Continent to continent
  • Slide 36
  • Ocean to ocean
  • Slide 37
  • TRANSFORM PLATE BOUNDARIES SAN ANDREAS FAULT MOVING TO NORTH/NORTHWEST AT A RATE OF 35 MILLIMETERS PER YEAR
  • Slide 38
  • transform
  • Slide 39
  • EARTHQUAKE VIBRATION OF THE EARTH PRODUCED BY THE RAPID RELEASE OF ENERGY ALONG FAULTS THIS ENERGY RADIATES OUTWARD FROM THE SOURCE OF THE QUAKE KNOWN AS THE FOCUS
  • Slide 40
  • focus
  • Slide 41
  • Elastic rebound
  • Slide 42
  • EPICENTER THE AREA ON THE EARTHS SURFACE IMMEDIATELY ABOVE THE FOCUS IT IS NOT THE SOURCE OF THE QUAKE
  • Slide 43
  • FAULTS PRODUCED BY THE NEVER ENDING MOVEMENT OF THE EARTHS CRUST FIND FAULTS AND EARTHQUAKES NEAR PLATE BOUNDARIES
  • Slide 44
  • Slide 45
  • OTHER QUAKES FORESHOCKS - QUAKES THAT PRECEDE THE MAIN EARTHQUAKE AFTERSHOCKS - QUAKES THAT FOLLOW THE MAIN EARTHQUAKE
  • Slide 46
  • EARTHQUAKE RECORDINGS SEISMOLOGY SEISMOGRAPH SEISMOGRAM RICHTER SCALE - LOGARITHMIC SCALE USED TO MEASURE THE ENERGY AND THE WAVE AMPLITUDE OF THE EARTHQUAKE
  • Slide 47
  • seismograph
  • Slide 48
  • seismogram
  • Slide 49
  • . ONE MILLION EARTHQUAKES OCCUR EVERY YEAR 6.0 OCCURS EVERY THREE DAYS ABOVE 8.0 ONCE EVERY 5/10 YEARS BELOW 2.5 ARE NOT FELT BUT CAN BE MEASURED
  • Slide 50
  • RICHTER SCALE INCREMENTS AN INCREASE OF 1.0 = A 10 TIMES INCREASE IN WAVE AMPLITUDE AND A 31.5 TIMES INCREASE IN ENERGY AN INCREASE OF 2.0 = A 100 TIMES INCREASE IN AMPLITUDE AND A 992.25 INCREASE IN ENERGY (31.5 X 31.5)
  • Slide 51
  • EARTHQUAKE WAVES SURFACE WAVES - TRAVEL ALONG EARTHS OUTER LAYER BODY WAVES - TRAVEL THROUGH EARTHS INTERIOR PRIMARY WAVES [P WAVES] - COMPRESS & EXPAND ROCKS IN THE DIRECTION WAVE TRAVELS SECONDARY WAVES [S WAVES] - SHAKE THE PARTICLES AT RIGHT ANGLES TO DIRECTION OF TRAVEL
  • Slide 52
  • pwave
  • Slide 53
  • swave
  • Slide 54
  • FINDING EARTHQUAKE EPICENTERS P WAVES ARRIVE AHEAD OF S WAVES. THE GREATER THE DISTANCE AWAY FROM EPICENTER THE LONGER THE TIME SPAN FROM P WAVE TO S WAVE. USE TRAVEL TIME GRAPHS FROM 3 OR MORE DIFFERENT STATIONS [TRIANGULATION] & THE INTERSECTING POINT IS THE EPICENTER
  • Slide 55
  • Finding epi
  • Slide 56
  • Epi circles
  • Slide 57
  • MERCALLI INTENSITY SCALE ASSESSES DAMAGE FROM A QUAKE AT A SPECIFIC LOCATION I - NOT FELT II - FELT ONLY ON UPPER FLOORS VI - HEAVY FURNITURE MOVED X - MOST FRAME STRUCTURES DESTROYED XII - DAMAGE TOTAL
  • Slide 58
  • PRECURSORS PHENOMENA THAT PRECEDE & THUS PROVIDE A WARNING OF A FORTHCOMING EARTHQUAKE UPLIFT, SUBSIDENCE, AND STRAIN IN THE ROCKS NEAR ACTIVE FAULTS PECULIAR BEHAVIOR
  • Slide 59
  • EARTHS INTERIOR STRUCTURE CORE - SOLID INNER MADE UP OF IRON AND LIQUID OUTER CORE MANTLE - LOWER IS A MIXTURE OF IRON, MAGNESIUM, AND SILICATES. UPPER MANTLE IS RIGID. UPPERMOST MANTLE IS WHERE THE LITHOSPHERE BEGINS CRUST - SOLID EARTH SURFACE
  • Slide 60
  • Earth structure
  • Slide 61
  • MOHOROVICIC DISCONTINUITY [MOHO] THE BOUNDARY SEPARATING THE CRUST FROM THE MANTLE, DISCERNIBLE BY AN INCREASE IN SEISMIC VELOCITY
  • Slide 62
  • LITHOSPHERE THE OUTERMOST RIGID UNIT [CRUST & UPPERMOST MANTLE] OF THE EARTH AVERAGING ABOUT 100 KILOMETERS [62 MILES] IN THICKNESS. THICKER OVER THE CONTINENTS & THINNER OVER THE OCEAN BASINS
  • Slide 63
  • ASTHENOSPHERE BENEATH THE LITHOSPHERE TO A DEPTH OF ABOUT 660 KILOMETERS [410 MILES]. TOP PART HAS MELTED ALLOWING LITHOSPHERE TO EFFECTIVELY DETACH FROM THE ASTHENOSPHERE BELOW IMPORTANT FOR PLATE TECTONICS THEORY
  • Slide 64
  • asthenosphere
  • Slide 65
  • CRUSTAL DEFORMATION FOLDING - THE COMPRESSION OF ROCK SYNCLINES ARE DOWNFOLDS OF ROCK ANTICLINES ARE UPFOLDS OF ROCK
  • Slide 66
  • folding
  • Slide 67
  • FAULTING FRACTURES IN ROCK INVOLVING DISPLACEMENT OF ROCK ON ONE SIDE WITH RESPECT TO THE OTHER A JOINT IS A FRACTURE WITHOUT DISPLACEMENT
  • Slide 68
  • NORMAL FAULT STRESSES PULL CRUSTAL ROCK APART CREATING MORE HORIZONTAL SPACE
  • Slide 69
  • Normal fault
  • Slide 70
  • REVERSE FAULT ONE BLOCK RIDING OVER THE OTHER COMPRESSING IT INTO SMALLER HORIZONTAL SPACE
  • Slide 71
  • Reverse fault
  • Slide 72
  • STRIKE SLIP FAULT HORIZONTAL MOVEMENT SUCH AS IN A TRANSFORM FAULT
  • Slide 73
  • Strike slip
  • Slide 74
  • CRUSTAL DEFORMATION FEATURES GRABEN - SUNKEN BLOCKS BETWEEN USUALLY PARALLEL NORMAL FAULTS AS IN A RIFT VALLEY HORST - A BLOCK RAISED BETWEEN REVERSE FAULTS
  • Slide 75
  • Graben and horst
  • Slide 76
  • HORST
  • Slide 77
  • GRABEN
  • Slide 78
  • VOLCANOES LAVA MAGMA PYROCLASTICS LAPILLI - WALNUT- SIZED CINDERS - PEA- SIZED BLOCK
  • Slide 79
  • LAPILLI
  • Slide 80
  • FACTORS DETERMINING TYPE OF ERUPTION MAGMAS COMPOSITION TEMPERATURE AMOUNT OF DISSOLVED GASES THESE FACTORS AFFECT THE MAGMAS VISCOSITY OR THICKNESS. MORE VISCOUS LAVA EQUALS MORE VIOLENT ERUPTION
  • Slide 81
  • WHERE DO WE FIND VOLCANOES? SUBDUCTION BOUNDARIES SEA FLOOR SPREADING CENTERS HOT SPOTS LOIHI
  • Slide 82
  • loihi
  • Slide 83
  • TYPES OF VOLCANIC ERUPTIONS EFFUSIVE ERRUPTIONS ARE GENTLE USUALLY CONSISTING OF LAVA. THEY PRODUCE SHIELD VOLCANOES WHICH ARE VERY BROAD GENTLY SLOPING CRATERS SUCH AS WE HAVE IN HAWAII
  • Slide 84
  • Shield volcano
  • Slide 85
  • . EXPLOSIVE ERUPTIONS CAN PRODUCE TWO TYPES OF VOLCANIC CONES. IF THE MATERIAL IS SOLELY PYROCLASTICS, A CINDER CONE IS PRODUCED. THIS IS A SMALL STEEPLY SLOPED CRATER
  • Slide 86
  • Cinder cone
  • Slide 87
  • IF THE ERUPTION ALTERNATES BETWEEN PRODUCING LAVA AND PYROCLASTICS, A COMPOSITE CONE OR STRATO VOLCANO IS PRODUCED. IN THESE THERE ARE ALTERNATING LAYERS OF LAVA AND PYROCLASTIC
  • Slide 88
  • Composite cone
  • Slide 89
  • LAVA TYPES PAHOEHOE - HOTTEST (2000 DEGREES F) AND HAS SMOOTH AND ROPEY TEXTURE AA - COOLER (1800 DEGREES F) AND IS JAGGED AND BLOCKY CLINKERS - 1600 DEGREES F, GETS ITS NAME FROM ITS SOUND
  • Slide 90
  • pahoehoe
  • Slide 91
  • aa
  • Slide 92
  • VOLCANIC FEATURES CALDERA (KETTLE) - BASIN SHAPED DEPRESSION - VALLE GRANDE IN NEW MEXICO OR CRATER LAKE, OREGON PACIFIC RING OF FIRE NUEE ARDENTE MT PELEE
  • Slide 93
  • Valle grande
  • Slide 94
  • .
  • Slide 95
  • PLUG DOMES VOLCANIC NECKS - SHIPROCK, NM DIKE RIDGE SILL LACCOLITH - A MASSIVE IGNEOUS BODY INTRUDED BETWEEN PRE-EXISTING STRATA BATHOLITH EROSION EXPOSED MASS LAHAR - MUDFLOWS
  • Slide 96
  • IGNEOUS LANDFORMS
  • Slide 97
  • Plug dome
  • Slide 98
  • Ship rock
  • Slide 99
  • SILL
  • Slide 100
  • batholith
  • Slide 101
  • TEST 2 REVIEW How will you do?
  • Slide 102
  • Fossils can be all but which of the following? A. Indirect Evidence B. Actual Remains C. Sedimentation D. Imprint Correct Response C. Sedimentation
  • Slide 103
  • 2. Which statement is true about the Earths crust? A. Continental rocks are heavier than ocean rocks B. Granite is a type of ocean rock C. Basalt is heavier than Granite D. Continental rocks are called sima Correct response C. basalt is heavier than granite
  • Slide 104
  • 3. Smaller-sized crystals are found in what type of rock? A. Intrusive B. Extrusive C. Silicates D. None of these Correct response B. extrusive
  • Slide 105
  • 4. Before it was a gneiss rock what was it? A. marble B. sandstone C. mica D. granite Correct response? D. granite
  • Slide 106
  • 5. The San Andreas fault is what type of boundary? A. divergent B. convergent C. transform D. Spreading center Correct response? C. transform
  • Slide 107
  • 6. Pahoehoe is? A. a jagged and blocky type of lava B. cooler than aa C. smooth and ropey textured lava D. the name of the new Hawaiian Island Correct response C. smooth and ropey textured lava
  • Slide 108
  • 7. Valle Grande & Crater Lake are examples of: A. calderas B. plug domes C. dike ridges D. laccoliths Correct response? A. calderas
  • Slide 109
  • 8. Iben Browning was famous for? A. his work in plate tectonics B. his work as a seismologist C. his faulty New Madrid prediction D. A & B are true Correct response? C. his faulty NM prediction
  • Slide 110
  • POSITIVE ASPECTS OF VOLCANIC ACTIVITY PRODUCES EXCELLENT AGRICULTURAL SOILS HELPS TO FORM METALLIC ORES PRODUCES GEOTHERMAL ENERGY ADDS GASES TO OUR ATMOSPHERE ADDS CONDENSATION SURFACES