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Earth`s Layers Song Lyrics
Earth`s Layers Song Lyrics

... About half of our planet’s mass. The mantle is composed of very hot dense rocks, That move and flow, always on the go, they never lock, Never stop, and they’re responsible for tectonic shift Please believe the Earth’s plates are adrift It’s pretty thick and the heat is awesome 1,600 at the top, 4,00 ...
Slide 1
Slide 1

... permanent magnet. However, magnetic fields such as those that surround the Earth can be produced by an electrical current. So, we think of the Earth now as a giant electromagnet. The electrical field is produced by the movement of electrons through the molten iron of the liquid outer core. ...
Minerals Mineral: naturally occurring inorganic solid that has a
Minerals Mineral: naturally occurring inorganic solid that has a

... 1. Earthquake: the shaking and trembling that result from the movement of rock beneath Earth’s surface. 2. Seismic waves carry the energy of the earthquake away from the focus, through Earth’s interior and across the surface. There are 3 categories of seismic waves; pwaves, s-waves, and surface wave ...
Chapter 6 - USD Home Pages
Chapter 6 - USD Home Pages

... Earth has an atmosphere. This burns up small meteoroids, but does not burn up large ones, which do strike Earth. The atmosphere also gives us weather, which gradually wears away craters. Tectonic motion also is constantly resurfacing the Earth. Meteor Crater in Arizona is about 50,000 years old, so ...
Lecture 17
Lecture 17

... Magmas have higher concentrations of some elements that most other rocks and depending on the cooling processes affecting the magma, very high concentrations of certain elements can occur. Basic transport – diamonds are carried to the surface/near surface by exotic ultramafic volcanic rocks from a s ...
Energy In The Rock Cycle
Energy In The Rock Cycle

... water harden sediments and __________ them together to form new rocks as water __________or moves away. • Chemical __________ within the earth’s crust __________rocks from one form to another. ...
Chapter 7 lessons 1,2 and 6 Review
Chapter 7 lessons 1,2 and 6 Review

... Mantle ( more specific include the parts of the mantel- optional) Lithosphere Asthenosphere Mesosphere Outer Core Inner Core ...
hotspots and magnetic reversals
hotspots and magnetic reversals

... records of reversals in the Earths magnetic field. ...
Plate Tectonics - MsPetersensScienceScholars
Plate Tectonics - MsPetersensScienceScholars

... 5. Click the white circles to see what kind of tectonic activity and geographic features go together. 6. Read the background information by clicking the “Background” tab at the bottom of the screen. 7. Answer the questions from the “Questions” tab in your ...
Ch. 14-Life History Lecture #1
Ch. 14-Life History Lecture #1

... V. The Age of a Fossil B. Radiometric Dating 1. Determination of how many of the original atoms are left in the rock. a. Atoms decay at a steady rate 2. Half-life- Time needed for ½ the atoms to decay a. If the fossil’s half-life is 2 million years, when ½ of its atoms are gone it will be 2 million ...
Week 30 CCA - Net Start Class
Week 30 CCA - Net Start Class

... objects. The strength of gravity depends on the mass of the objects and the distance between them. There is gravity between a moon and its planet. 9. Explain how mass and gravitational pull related? Greater the mass the stronger the gravitational pull 10. How has the Hubble Telescope been the most u ...
Journey to the Center of the Earth Project - Science
Journey to the Center of the Earth Project - Science

... b. Continental crust c. Oceanic crust d. Lithosphere e. Asthenosphere f. Mantle g. Inner core h. Outer core 2. Label each of the above parts of the model. Part 2 - Write a short story to go along with your model. The story is about a scientist (maybe you???) traveling to the center of the Earth. Beg ...
Slide 1
Slide 1

... • Today, some buildings are made of more flexible materials so that they bend and sway during an earthquake and do not fall down as easily. • We are going to experiment with different “building materials” and see which are the ...
Converging Plate Boundaries
Converging Plate Boundaries

... Converging Plate Boundaries From “This Dynamic Planet” by USGS ...
Questions for Battle Ball
Questions for Battle Ball

... 2. What do the plates of the lithosphere float on? 3. The hypothesis that continents have slowly moved to their current location is called what? 4. What plate movement happens at divergent plate boundaries? 5. What plate movement happens at convergent plate boundaries? 6. What plate movement happens ...
lesson 1 and water - Warren County Schools
lesson 1 and water - Warren County Schools

... Deforming the Earth's Crust Chapter 4 Lesson 4 ...
11.30-plate-tectonics
11.30-plate-tectonics

... • Found evidence of similar fossils and geological formations on different continents • The shape of continents also seemed to “fit” together ...
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY

... Reverse Thrust? Transform/Transcurrent Fault? How are faults formed? What forces are at work? Can you give an example of Fault Block Mountains? Can you give an example of Folded Mountains? What are Earthquakes? What are: P-waves, S-waves? How does the Epicenter differ from the Focus (hypocenter)? Wh ...
Activity 3
Activity 3

... 16. Mars has the largest volcanoes in the solar system. Olympus Mons is over 20km high; nothing on the Earth (volcanic or otherwise) even comes close to this. The main reason Mars can have such high mountains is… a) Due to its weaker gravity which lowers the weight of the mountain b) Due to its col ...
Page 1 UNIT 2 - Earthquakes Handout 4 Sources: www.britannica
Page 1 UNIT 2 - Earthquakes Handout 4 Sources: www.britannica

Causes of Plate Movement
Causes of Plate Movement

... Magma that is hotter is less dense and rises. As it moves, it pulls a lithospheric plate with it ...
Day-29
Day-29

...  Volcanism is related to tectonism and is a sign of geologic activity.  The movement of the tectonic plates generates a lot of thermal energy from friction.  This energy combines with heat from convection cells in the mantle to heat portions of the lower crust and upper mantle as magma. ...
Lithospheric
Lithospheric

... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
Chapter 3 The Origin of Ocean Basins LEARNING OBJECTIVES 1
Chapter 3 The Origin of Ocean Basins LEARNING OBJECTIVES 1

What is the theory of plate tectonics
What is the theory of plate tectonics

... Crust - The crust is Earth’s thin, outermost layer. __________________ is thick and made of low-density rock, such as granite. ________ crust is thin and made of denser rock, such as basalt. Mantle -The mantle is made of dense, _______________ minerals. Core - The Earth’s core is a hot, dense sphere ...
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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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