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5. Seismology and Plate Tectonics
5. Seismology and Plate Tectonics

... p vectors and transform faults lie on small circles about the pole, the pole must lie on a great circle at right angles to them. ...
class outline - WordPress.com
class outline - WordPress.com

... C. A tectonic plate consists of the crust and the top layer in the mantle. D. A tectonic plate is made up of Earth’s outer layer that is found in the upper mantle. E. A tectonic plate is a rigid layer of Earth that moves in the asthenosphere. F. A tectonic plate is lithosphere. ...
Forces Within Earth
Forces Within Earth

... • Normal faults are fractures caused by horizontal tension. • Strike-slip faults are fractures caused by horizontal shear. ...
The Layer`s Of The Earth!
The Layer`s Of The Earth!

... energy suddenly created by the breaking up of rock within the earth or an explosion .They are the energy that travels through the earth and is recorded on seismographs. ...
Eliana
Eliana

... My team and I, Eliana Monaghan, have fulfilled your request to answer the following questions: Where are the most recent earthquakes occurring, and are they more likely to occur in certain locations? Are there parts of the world that are more prone to them? Is there a relationship between earthquake ...
How accurately can we measure density within the Earth?
How accurately can we measure density within the Earth?

... depth ...
Earthquakes and the Interior
Earthquakes and the Interior

...  P-waves are bent (refracted) at the mantle-outer core boundary and bend deeper into the outer core. This causes these P-waves to arrive at Earth’s surface some distance away from P-waves that do not travel through the Outer core. ...
Earthquakes Terminology of Earthquakes Elastic Rebound Theory
Earthquakes Terminology of Earthquakes Elastic Rebound Theory

... exceeds the strength of the rock and it fractures. • The stored elastic strain energy is rapidly released and propagates outward as vibration waves called seismic waves. ...
Structure of the Earth
Structure of the Earth

... Continental lithosphere is very different from oceanic lithosphere. To understand this, we need to know more about the structure & composition of Earth. ...
Chapter 8 Earthquake Notes
Chapter 8 Earthquake Notes

... • What are 3 basic types of faults? • What equipment is used to record/measure earthquakes? • What is the center of the earthquake called? How do we locate it? • What are the different types of quake waves? What are their characteristics? • Describe the scale used to measure quakes. ...
the layers of the earth - NATSCI-A7
the layers of the earth - NATSCI-A7

... locating ...
Google Earth Plate Boundaries Activity Materials
Google Earth Plate Boundaries Activity Materials

... plates. The Arabian plate is already rifted off, creating the Red Sea. **This boundary is not marked in the USGS provide Plate Boundary file, but is in the plate_boundaries.kml made by various researchers. 7. Extra #1 – Another Ocean-Continent Convergent Boundary: Mt. St. Helens 46.191°N 122.194°W. ...
Rheology Thoughts
Rheology Thoughts

... infuse one or more of the course topics with an understanding of the processes behind the mathematical descriptions of material behavior and/or with a feel or intuition for selecting one or more behaviors for earth materials experiencing geophysical events or characterization. The format will be to ...
Field Notebook
Field Notebook

... Submit by Email ...
Example or Rigor
Example or Rigor

... earthquakes/volcanoes and what type of damage they ...
Can Humans Travel to the Center of the Earth?
Can Humans Travel to the Center of the Earth?

class outline - WordPress.com
class outline - WordPress.com

... by oceanic trenches and are located toward the center of most ocean basins. An oceanic ridge would have the youngest ocean floor in a typical ocean basin. As the oceanic lithosphere spreads away from the divergent boundary, the age of rocks on the ocean floor get older and older. Oceanic lithosphere ...
File - Mr. Carter`s Earth
File - Mr. Carter`s Earth

... 4. Compare and contrast the outdated Richter scale and more precise moment magnitude that are used to measure earthquakes. Give 2 differences. a. ...
Ambient Noise Tomography
Ambient Noise Tomography

Earthquakes
Earthquakes

... • Many subduction zone quakes are deep – up to 700 km deep • This point below the surface where the plate actually slips or snaps is called the FOCUS ...
PDF file of Lecture 4a - Earth`s Interior and Tectonics
PDF file of Lecture 4a - Earth`s Interior and Tectonics

... Earthquake zones, volcanism, and mountain building (tectonic activity)  plate boundaries ...
Modelling and Analysis of the Earthquake Zones of British
Modelling and Analysis of the Earthquake Zones of British

... Anisotropy is expected with the shifting of continental plates which are meant to have a directional flow that is determined by the different methods of calculations available. Calculations using the inverse distance weighting method will suffice for many anisotropic studies. This method calculates ...
How stress transfer between volcanic and seismic zones af
How stress transfer between volcanic and seismic zones af

... northeast and southwest quadrants and compressive in the northwest and southeast quadrants. These model results agree with observations made when the SISZ was loaded to failure in June 2000, resulting in two M6.6 earthquakes. For several years prior to the June 2000 earthquakes, compression, uplift ...
earthquake
earthquake

...  Long-Range Forecasts • Scientists don’t yet understand enough about how and where earthquakes will occur to make accurate long-term predictions. • A seismic gap is an area along a fault where there has not been any earthquake activity for a long period of time. ...
Geology 120 Problem Set #3 Ch. 8-10 due 3/16 Metamorphic Rocks
Geology 120 Problem Set #3 Ch. 8-10 due 3/16 Metamorphic Rocks

... 1. Describe how the scientific ideas about geologic has changed in the last 200 years. 2. Explain the six fundamental principles of relative dating. 3. How does and unconformity develop? What are three different types? 4. If you want to calculate the absolute age of an intrusive igneous rock, what i ...
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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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