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Chapter 12 Thermal Energy Transfer Drives Plate Tectonics 12.1
Chapter 12 Thermal Energy Transfer Drives Plate Tectonics 12.1

... climates, (eg. Such as ___________________) on warm continents. Act. 12-1C – Piecing Together Pangaea 2. How Can Continents Move? • Wegener’s evidence for continental drift did ___________________  New scientific equipment _________________.  It was noted that ___________________ appear in certain ...
First Quarter Exam Review Sheet Name
First Quarter Exam Review Sheet Name

... What has to happen to make a sedimentary or metamorphic rock change into an igneous rock? How can crystal size be used to determine where igneous rocks formed? Describe how rocks with small fragments (bits and pieces) probably formed. What causes earthquakes? What is the lag time between P and S wav ...
Poster list
Poster list

... Evidence  of  Cascadia  Earthquakes  in  Lacustrine  Sediments High  precision  Sr-­‐Nd-­‐Hf-­‐Pb  isotopic  data  on  northern  Cascade  arc   basalts  reveal  spatial  gradients  in  mantle  source  compositions  and   subducting  sediment  input ...
Thermal Convection and Viscosity…
Thermal Convection and Viscosity…

... 2. Next, make a cube out of a piece of silly putty. The silly putty can be thought of as an elastic solid for short-duration stresses (if you roll it into a ball, it will bounce off the floor, similar to a rubber ball, if dropped), and a viscous fluid for longer time processes (note also the viscosi ...
Discovering Plate Boundaries
Discovering Plate Boundaries

... 3. Transform-Fault Boundaries •Volcanos dispersed, most on one side •Earthquakes complex, shallow (to medium) on both sides •Age data not symmetrical, one side of boundary •Complex topography, wide mountains and basins •Rocks? ...
Plate Motions Activity
Plate Motions Activity

... Plate Tectonics explains how the earth’s lithosphere has evolved over geologic time. This theory explains why the Pacific Northwest has earthquakes and volcanoes and Louisiana does not. It also explains how and when major mountain ranges (e.g., Rocky Mountains) or ocean basins (e.g., Gulf of Mexico) ...
8 The dynamic Earth
8 The dynamic Earth

Layers of the Earth Project
Layers of the Earth Project

... A short creative story about traveling to the center of the earth or a story about experiencing an earthquake or the Earth’s magnetic field. If about traveling to the center of the earth, start on the Crust and describe your journey as you travel through each layer. What do you see? How do you feel? ...
Understanding Plate Boundaries
Understanding Plate Boundaries

... 2. On Student Sheet 44.2, “Plate Boundaries,” you drew the boundaries of large, lithospheric plates. Use information from this reading to identify and label: a. a transform boundary b. a divergent boundary c. a convergent boundary 3. Yucca Mountain is located close to H6 on Student Sheet 44.2. Which ...
Plate Tectonics study guide
Plate Tectonics study guide

... 12. The oceanic crust is denser than the continental crust. That is why the oceanic crust sub ducts under the continental crust. Fill in the blanks 13. Two continental crust colliding can create mountains 14. Divergent boundaries can be caused by convection currents in the mantle. 15. folding in the ...
ES 104 Midterm Exam Study Guide 1
ES 104 Midterm Exam Study Guide 1

... Know the difference between earthquake intensity and magnitude. Know how an earthquake’s magnitude is determined on the Richter’s Scale. Know that each number on the Richter’s scale corresponds with a 32-fold increase in energy released during an earthquake. Know how an earthquake’s moment magnitude ...
Precambrian Rohbaugh
Precambrian Rohbaugh

... • Hadean: Lots of carbon dioxide, water vapor and methane • Archean: Water vapor forms oceans, oxygen starts to be made by photosynthetic organisms • Proterozoic: Significant oxygen in atmosphere, massive drop in carbon dioxide ...
Water | CALS Cooperative Extension
Water | CALS Cooperative Extension

... to the strike (direction) of the plate boundary. This stretching is evident in the alignment of mountain peaks and valleys in a general northwest – southeast alignment pattern, referred to geologically as lineation. As the earth’s crust is stretched, blocks of crust break and drop in a pattern of va ...
Volcanoes Pre-lab Lesson Plan
Volcanoes Pre-lab Lesson Plan

...  Lithosphere: The Earth's hard, outermost shell. It comprises the crust and the upper part of the mantle and is divided into a mosaic of 16 major slabs, or plates. These plates float on top of the asthenosphere, a more plastic layer in the Earth's mantle.  Magma: Molten rock containing liquids, cr ...
Plate Tectonics and Mountain Building – Study Guide Plate
Plate Tectonics and Mountain Building – Study Guide Plate

... 6. According to the theory of plate tectonics, the __________________ was divided into _________ 7. What kind of plate boundary occurs where two plates grind past each other without destroying or producing lithosphere? 8. A divergent boundary at two oceanic plates can result in a ____. 9. What type ...
Convergent Boundaries
Convergent Boundaries

... ◦ This is what causes tectonic plates to move around. ...
HERE
HERE

... location of earthquakes, volcanoes, and midocean ridges; and the distribution of fossils, rock types, and ancient climatic zones. b. Students know Earth is composed of several layers: a cold, brittle lithosphere; a hot, convecting mantle; and a dense, metallic core. c. Students know lithospheric pla ...
Earth Science Chapter 21: Fossils and the Rock Record Chapter
Earth Science Chapter 21: Fossils and the Rock Record Chapter

... Distinctive rock layers that extend over large areas can be dated by radiometric dating techniques then become time markers called key beds and can be used to date rock layers above and below them Section 4: Fossil Remains Fossils are the evidence or remains of once-living plants or animals. They pr ...
Cornell Notes Topic/Objective: The Theory of Plate Tectonics Name
Cornell Notes Topic/Objective: The Theory of Plate Tectonics Name

... Essential Question: What is the theory of plate tectonics? What are the three types of plate boundaries? ...
Mesozoic Plate Tectonics
Mesozoic Plate Tectonics

... At the end of the Paleozoic, there was one continent and one ocean. Then Pangaea began to break apart about 180 million years ago. The Panthalassa Ocean separated into the individual but interconnected oceans that we see today on Earth. Continental rifting and then seafloor spreading pushed Africa a ...
43-48 Ma - EPSc 453 Interior of the Earth
43-48 Ma - EPSc 453 Interior of the Earth

... • Total heat flow of the earth is 46 TW, 38 TW emerges from the mantle • Plume flux is only a small part of heat transport relative to plate tectonics and large-scale convection ...
Ch. 11 Coastal Ocean - Seattle Central College
Ch. 11 Coastal Ocean - Seattle Central College

... What are 4 fields that contribute to our understanding of oceans? Describe the sorts of information we get from each field and a few of the concerns of each. ...
No Slide Title
No Slide Title

... • Such a configuration exerted tremendous influence on the world's climate – resulted in generally arid conditions over large parts of Pangaea's interior ...
chpt 7Plate Tectonics
chpt 7Plate Tectonics

... transform boundaries are result where two plates slide past each other  They move in opposite direction and usually earthquakes are associated with transform boundaries  San Andreas fault is an example ...
Discuss on Sea Floor Evidence Submitted by WWW
Discuss on Sea Floor Evidence Submitted by WWW

... floor spreading were supported by reliable scientific data and combined to develop modern‐day plate tectonic theory. The theory maintains that the crust and uppermost mantle, or lithosphere, is segmented into a number of solid, rigid slabs called lithospheric plates. These slabs move slowly over the ...
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Geophysics



Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
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