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Oregon Corvallis Why is there a green side and a brown side of Oregon? Oregon Why are there Two Parallel Mountain Ranges in Oregon? The Whole Earth and Plate Tectonics We need to understand know what goes on inside the Earth. Depths in Miles Oreo® Cookie Oreo® Cookie Oreo® Cookie Oreo® Cookie Oreo® Cookie Oreo® Cookie Oreo® Cookie ® Oreo Psycho-Personality Test www.superkids.com/aweb/pages/humor/050199.sht • Psychologists have discovered that the manner in which people eat Oreo® cookies provides great insight into their personalities. Choose which method best describes your favorite method of eating Oreos: • 1. The whole thing at once. 2. One bite at a time. 3. Slow and methodical nibbles examining the results of each bite afterwards. 4. In little feverous nibbles. 5. Dunked in some liquid (milk, coffee …..) 6. Twisted apart, the inside, then the cookie. 7. Twisted apart, the inside, and toss the cookie. 8. Just the cookie, not the inside. 9. I just like to lick them, not eat them. 10. I don’t have a favorite way because I don’t like Oreos. 6. Twisted apart, the inside, then the cookie. • You have a highly curious nature. • You take pleasure in breaking things apart to find out how they work, though you’re not always able to put them back together, so you destroy all the evidence of your activities. • You deny your involvement when things go wrong. • You are a compulsive liar and exhibit deviant, if not criminal, behavior. Sliding Plate over Asthenosphere Parks and Plates, ©2005 Robert J. Lillie North America Parks and Plates ©2005 Robert J. Lillie Atlantic Ocean Africa Divergent Plate Boundary Iceland North America Africa Iceland Pillow Basalt New lithosphere created at divergent plate boundaries. Does that mean Earth is expanding? Mid-Atlantic Ridge Atlantic Ocean South America Divergent Plate Boundary: New Lithosphere Created Africa Asthenosphere Trench Lithosphere Lower Mantle Convergent CorePlate Boundary: Lithosphere Recycled back into Deeper Mantle Deep-Sea Subducting Trench Plate Overriding Plate Parks and Plates ©2005 Robert J. Lillie Convergent Plate Boundary Coast Range Cascades Subduction of the Juan de Fuca Plate forms the Coastal Ranges and Cascade Volcanoes Formation of the two parallel mountain ranges. Sedimentary layers scraped off the subducting plate form the Coast Range. Corvallis, Oregon Mary’s Peak Oregon State University Pillow Basalt – Coast Range Rocks made in the Ocean! Mary’s Peak Just like when you bicycle, the subducting plate sweats when it gets hot The rising hot water melts rock in its path, forming magma. Mount Hood and other Cascade Volcanoes form where some of the magma reaches the surface. Puget Sound and the Willamette Valley are low-lying regions between the rising mountains. Mt. St. Helens, Washington Steep Composite Volcano Prior to 1980 Mt. St. Helens, Washington Bulge on North Side of Mountain Early 1980 Mt. St. Helens, Washington Explosive Eruption May 18, 1980 Mt. St. Helens, Washington Eruption Cloud May 18, 1980 Mt. St. Helens National Volcanic Monument, Washington 200 + foot Douglas Fir trees downed on north side of mountain Mt. St. Helens National Volcanic Monument, Washington 7,700 years ago – Southern Oregon’s Mt. Mazama was perhaps taller than Mt. Hood. Vast amounts of volcanic ash, pumice, and lava flows erupted – the top of the mountain collapsed as rubble to fill the void, creating a large crater. No rivers or creeks flow in or out of Mt. Mazama’s crater – rainfall and snowmelt partially fill it with some of the purest and clearest water in the world Crater Lake – 1,943 feet (592 meters) – deepest in the United States and 7th deepest in the world! Later eruptions coated the crater floor – just like at Aniakchak Volcano in Alaska! Lava Flows Volcano Inside a Volcano Aniakchak National Monument, Alaska Lava flows seal the bottom of Crater Lake Volcano Inside a Volcano Wizard Island Merriam Cone Lava Flows Crater Lake FlyThrough Movie Time: 0:57 U.S. Geological Survey 3-D Image of Lake Bottom Wizard Island is a Cinder Cone Volcano formed after Mt. Mazama collapsed Wizard Island Oregon The Two Parallel Mountain Ranges make the green and brown sides of Oregon There are 20 potentially active volcanoes in the western United States (excluding Alaska and Hawaii). Half are in the Cascades of Washington, Oregon, and northern California. Cracked Egg Shell! Parks and Plates ©2005 Robert J. Lillie Western California is a Transform Plate Boundary San Andreas Fault Plate Boundaries Parks and Plates ©2005 Robert J. Lillie San Andreas Pacific Fault Plate North American Plate Transform Plate Boundary Parks and Plates ©2005 Robert J. Lillie Creating the SAN ANDREAS FAULT with a Deck of Cards Pretend your left hand is the Pacific Plate, your right hand the North American Plate. Parks and Plates ©2005 Robert J. Lillie Creating the SAN ANDREAS FAULT with a Deck of Cards The TRANSFORM PLATE BOUNDARY is a broad zone of shearing between the two plates. Parks and Plates ©2005 Robert J. Lillie Creating the SAN ANDREAS FAULT with a Deck of Cards One card face eventually takes over, simulating the predominance of movement along the San Andreas Fault. Parks and Plates ©2005 Robert J. Lillie So in 100 years, a total of 17 feet (5 meters) of movement would occur across the fault! 2 inches/year x 100 years = 200 inches = 17 feet! Orange Grove in Southern California – Planted 100 Years Ago The San Andreas Fault and Gulf of California accommodate transform plate motion between the North American and Pacific plates. The San Andreas Fault accommodates most of the transform plate motion in California. Parks and Plates ©2005 Robert J. Lillie California Earthquake 1973 Earthquakes Most earthquakes are at plate boundaries. Parks and Plates ©2005 Robert J. Lillie Plate Boundaries Parks and Plates ©2005 Robert J. Lillie Where are the Volcanoes? Earth has more than 1500 active volcanoes 70% of them are in the "Ring of Fire" Turcotte, 1971 Plate Boundaries Cascadia Subduction Zone 1. Where do Big Earthquakes occur? Plates stick together for about 300 years, then suddenly let go! Boom!!!! 2. Why do they occur there? Locked Zone Earthquake in the Pacific Northwest Parks and Plates ©2005 Robert J. Lillie Locked Zone Earthquake in the Pacific Northwest Parks and Plates ©2005 Robert J. Lillie What drowned these trees 300 years ago? U.S.G.S. Generation of a Tsunami Earthquakes from under the seas Cause big waves to submerge the trees The first waves are small Compared to them all These waves we call – tsunamis! Cascadia Subduction Zone We can see what’s on the surface. How does the surface change when the plates are stuck? How do we really know what’s beneath here? EarthScope A project to: – Explore the structure and evolution of the North American continent – Understand processes that cause earthquakes and volcanic eruptions. Drillhole across San Andreas Fault 875 GPS Instruments 175 Borehole Strainmeters 5 Long-Baseline Laser Strainmeters 400 Seismometers at 2,000 sites 100 Permanent Seismometers