Plate Tectonics
Rigid, rocky outer surface of the Earth Definition Tectonic: Plate: Rigid, rocky outer surface of the Earth To build or destroy The processes by which the rocky plates of the planet move and interact with each other
Internal Structure of the Earth lithosphere plates mantle inner core hot dense rock solid iron outer core liquid iron
Lithospheric Plates Continental: Oceanic: thick, light, mostly granite thin, heavy, mostly lava flows Asthenosphere Weak, plastic upper mantle
Lithospheric Plates
Diverging Plate Boundaries Where plates pull apart from each other Stretching & thinning High heat flow (New Crust Created)
Diverging Plate Boundaries Key landform: mid-oceanic ridges volcanic mt. ranges axial valley 1000’s miles long 1-2 miles tall
Converging Plate Boundaries Where plates collide Subduction zone: collision between oceanic and continental lithosphere (Crust Destroyed)
trenches & volcanic arcs Subduction zones Key landforms: trenches & volcanic arcs
Transform Plate Boundaries Where plates slide side by side Key landform: faults (Crust neither destroyed or created)
thermal convection / convection currents plate sinks and subducts Driving Force thermal convection / convection currents pushes up at ridges plates spread away hot rock cold rock plate sinks and subducts
Geologic activity at plate margins Volcanism: C, D Earthquakes: C, D, T Rock Deformation: C, D, T
Evidence: shape of continents The margins of some continents look like they could fit together First proposed by Alfred Wegner
Fossil Evidence
Nonrandom occurrence of volcanic activity Evidence: volcanoes Nonrandom occurrence of volcanic activity
Evidence: earthquakes Nonrandom occurrence of earthquakes Shallow at diverging margins deep at converging margins
Stationary upwellings of heat away from plate margins Evidence: hot spots Stationary upwellings of heat away from plate margins
Evidence: hot spots As plates move, the volcanoes are carried away from the hot spot Only volcanoes near the hot spot are are active Can determine direction and speed of the plate motion
Evidence: age of seafloor rocks Youngest rocks are found at the mid oceanic ridges Oldest rock are found farthest from the ridge
Evidence: paleomagnetism Earth has a strong magnetic field Iron rich volcanic rocks record Earth’s magnetic field at the time they form
seafloor paleomagnetic record Bands of alternating polarity Symmetrical about the mid oceanic ridges
seafloor paleomagnetic record lava forming at the ridges picks up the current magnetism, then gets pushed out of the way as newer lava forms Records of the growth and spreading of the seafloor
seafloor paleomagnetic record The alternating polarity represents complete reversals of Earth’s magnetic field
continental paleomagnetic record The location of magnetic poles on separate continents appear to wander with time If the poles haven’t moved significantly, then the continents did Use overlapping poles to reconstruct the past positions of the continents
Plate Tectonics in the PNW Cascadia subduction zone
Plate Tectonics in the PNW Cascades volcanic arc
Plate Tectonics in the PNW Juan de Fuca & Gorda mid ocean ridges
Plate Tectonics in the PNW Blanco & Medocino fracture zones
Plate Tectonics in the PNW “exotic terranes islands carried by the plates Attached to the North America continent
seafloor paleomagnetic record Bands of alternating polarity Symmetrical about the mid oceanic ridges
Evidence: paleo-environments
Evidence: distribution of mountains
Importance of Plate Tectonics