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presentation
presentation

... Earth structure: The main units • Crust versus mantle: The crust is a product of mantle melting. Typical mantle rocks have a higher magnesium to iron ratio, and a smaller portion of silicon and aluminum than the crust. • Lithosphere versus asthenosphere: While the lithosphere behaves as a rigid bod ...
Unit 1 topic 1 revision
Unit 1 topic 1 revision

... Compare volcanoes Mount Nyiragongo Mt St Helens Dem. Rep. of Congo - Africa USA Developing Developed Constructive - plates pulling Destructive – subduction (OC under CC) apart Runny basalt lava, not explosive Very explosive, little lava, ash, pyroclastic flow 57 died, evacuated area, US 100 died, 12 ...
Earth Sciences 11 - BC Curriculum
Earth Sciences 11 - BC Curriculum

Ch 9 study guide answer key
Ch 9 study guide answer key

... Which one of the following was NOT used as support of Wegener’s continental drift hypothesis? a. fossil evidence c. the fit of South America and Africa b. Paleomagnetism d. ancient climates ...
earthquakes - FacultyWeb Support Center
earthquakes - FacultyWeb Support Center

... 1. anticline--a fold arching upward 2. syncline--a fold arching downward 3. limb--sides of a old 4. fold axis—a line dividing the two limbs of a fold and running along the crest of an anticline or the trough of a syncline a. plunge: when the axis in inclined or tipped at an angle b. plunging fold: a ...
Document
Document

... Earth structure: The main units • Crust versus mantle: The crust is a product of mantle melting. Typical mantle rocks have a higher magnesium to iron ratio, and a smaller portion of silicon and aluminum than the crust. • Lithosphere versus asthenosphere: While the lithosphere behaves as a rigid bod ...
MYSTERIES OF PLANET EARTH
MYSTERIES OF PLANET EARTH

... Seismograph- device that measures the magnitude of earthquake  Seismogram is visual record of arrival time and magnitude of shaking associated with seismic wave ...
LETTERS Space geodetic evidence for rapid strain rates in the
LETTERS Space geodetic evidence for rapid strain rates in the

... earthquake focal mechanisms (Fig. 1). These sites are separated by a fault-normal distance of ,7 km and show a relative fault-parallel right-lateral velocity of ,1 mm yr21. In each case, the relative velocities yield current strain rates of the order of 1027 yr21. These rates are comparable to those ...
Chapter 8 Study Guide – Earthquakes 1. What is an earthquake
Chapter 8 Study Guide – Earthquakes 1. What is an earthquake

... P-waves: “push-pull” waves, they compress and expand rocks in the direction that waves travel S-waves: shake particles at right angles to their direction of travel Surface waves: up and down motion as well as side-to-side motion Strongest: surface waves  body waves (P- and S-waves) : Weakest Fastes ...
Pangaea
Pangaea

... What information did scientists study in order to develop this model? Many scientists believe that crustal plate movement occurs because of convection cells contained in Earth’s ...
Subsurface Research Group
Subsurface Research Group

... societal relevance, now depend critically on the integration of information and insights from three hitherto traditionally separate fields. These are: the physics and chemistry of Earth materials and fluids; real-time observations of the Earth’s response to stress, material and heat transfer through ...
S Ch 4 Earthquakes and Volcanoes NOTES
S Ch 4 Earthquakes and Volcanoes NOTES

... A) Measures the amount of _____________ that an earthquake releases 1) Each number of magnitudes is __x stronger than the number below it. ...
Seismicity, crustal structure, and morphology of the Louisville Ridge
Seismicity, crustal structure, and morphology of the Louisville Ridge

... overthrusting Indo-Australian and subducting Pacific plates. We have found in previous studies, for example, that seamounts of the type that make up the Louisville Ridge may act as either a barrier or asperity during large subduction zone earthquakes. Shallow earthquakes for the period 1964-present ...
Plate Tectonics
Plate Tectonics

... – Explains the formation, movement, and subduction of Earth’s plates How Plates Move: Theory of Plate Tectonics • _____________________rides on top of the ________________________________ • ________________________ride on top of mantle which is in motion due to _________________________ – Convectio ...
Discovering Plate Boundaries
Discovering Plate Boundaries

... Goal: Students will be able to explain and justify conclusions based on data, maps, and diagrams about the formation and boundaries of geologic features due to tectonic plate movement. Background: The Earth’s outermost layer is fragmented into plates that are moving relative to one another as they s ...
PPT file
PPT file

... These Back-Arc Basins are closely related to the subduction zone/Island arc systems found in the western part of the Pacific ocean and have also been found to have hydrothermal vent activity and have a rich biosphere surrounding those hydrothermal vents. ...
Why Do Earthquakes Happen?
Why Do Earthquakes Happen?

... the evolution of the Earth they signal the geological forces that build our mountains and create our oceans. In many ways, earthquakes are one of nature’s reminders that we are living on the thin outer crust of a planet whose interior is still cooling. Earthquakes happen when parts of Earth’s crust ...
The Earth`s Layers and Plate Tectonics Study Guide #1 Unit 3
The Earth`s Layers and Plate Tectonics Study Guide #1 Unit 3

... Support for Continental Drift Theory Continents seemed to fit together like puzzle pieces He found similar fossils on continents that are thousands of miles away from each other •similar sequence of rocks at numerous locations •plant fossils found in Antarctica which suggested that Antarctica was on ...
I Can
I Can

... I can describe how scientific innovations have been applied for use in our society and culture. SC.O.E. 1.9 I can use science to explore the natural world (form, function, systems, and changes over time). ...
Chapter 3: EARTH STRUCTURE AND PLATE TECTONICS
Chapter 3: EARTH STRUCTURE AND PLATE TECTONICS

... As we saw in the chapter, recent research has shown that slabs of Earth's relatively cool and solid surface—its lithosphere—float and move independently of one another over the hotter, partially molten asthenosphere layer directly below. The physical properties of each make this possible, so classif ...
Quiz - SLH PD Earthquakes
Quiz - SLH PD Earthquakes

... Inside the Earth We believe the Earth is divided into layers comprised of the crust, upper mantle, mantle and outer and inner core. This model explains the Earth’s tectonic plate movements and other phenomena, such as our magnetic field. But how did we arrive at this model? Moulding the Earth When s ...
Plate Tectonics Vocabulary Continental Drift The
Plate Tectonics Vocabulary Continental Drift The

... of continental and oceanic crust The theory that pieces of Earth’s lithosphere are in constant motion , driven by convection currents in the mantle A deep valley that forms where two plates move apart The process by which molten material adds new oceanic crust to the ocean floor A system that determ ...
Elasticity and Anisotropy of Common Crustal Minerals
Elasticity and Anisotropy of Common Crustal Minerals

... rich plagioclase. If this rock was isotropic the lines would all be flat because they would not change with direction. ...
DATASHEETforHANDOUTB
DATASHEETforHANDOUTB

... 3. What are two strengths for using Graham Crackers, chewing gum and frosting for a model for understanding how plates move and the theory of Plate Tectonics? ...
Accommodating sill-complex emplacement
Accommodating sill-complex emplacement

... forced folds, sub-horizontal sills may evolve into laccoliths or obtain a saucer-shaped morphology. These analyses highlight that the behaviour of the host rock during emplacement strongly influences forced fold evolution and may also determine whether additional space-making mechanisms occur (e.g., ...
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Earthscope



Earthscope is an earth science program using geological and geophysical techniques to explore the structure and evolution of the North American continent and to understand the processes controlling earthquakes and volcanoes. The project has three components: USARRAY, the Plate Boundary Observatory, and the San Andreas Fault Observatory at Depth.The project is funded by the National Science Foundation (NSF), and the data produced is publicly accessible in real-time. Organizations associated with the project include UNAVCO, the Incorporated Research Institutions for Seismology (IRIS), Stanford University, the United States Geological Survey (USGS) and National Aeronautics and Space Administration (NASA). Several international organizations also contribute to the initiative.
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