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Lesson Plan - ScienceA2Z.com
Lesson Plan - ScienceA2Z.com

... scale motions of the Earth's lithosphere. The theory encompassed and superseded the older theory of continental drift from the first half of the 20th century and the concept of seafloor spreading developed during the 1960s. The outermost part of the Earth's interior is made up of two layers: above i ...
ES Notebook Pages
ES Notebook Pages

... • The International Date Line is 180 o longitude (halfway around the Earth from the Prime Meridian, halfway between China and California in the middle of the Pacific Ocean). It is the highest number that can be used for longitude and it doesn’t need an East or West label. • Meridians are closer toge ...
Printer-friendly Version
Printer-friendly Version

THE BIG EVENT Oceans Fact Sheet
THE BIG EVENT Oceans Fact Sheet

... of certain features that rise above the water's surface as islands. The oldest rocks in the ocean date back only 200 million years, quite young for a planet thought to be about 4.5 billion years old. New crust constantly rises to the ocean surface along the mid-ocean ridge system, a giant underwater ...
Origin of the Earth`s Crust and its Evolution
Origin of the Earth`s Crust and its Evolution

... eu--geosynclinal deposits, non-marine in origin, are extensively known. It is accordingly not important problem in this concern, whether or not the geosynclinal deposits were built under the sea water, Eventually, the depositional basin became mountain, and sediments including volcanics turned into ...
density lab pictures and explanation
density lab pictures and explanation

... g/cm3 , respectively; remember that you have measured the density of only one sample of each type of rock). Both overlie the earth’s mantle which is denser (3.3 g/cm3), with the continental crust “floating “ higher. Understanding the differences between oceanic and continental crust is crucial for u ...
SeiSmological grand challengeS in UnderStanding earth`S
SeiSmological grand challengeS in UnderStanding earth`S

GEO 1010 - I 1. 2. 3. 4. - Research at UVU
GEO 1010 - I 1. 2. 3. 4. - Research at UVU

... A large earthquake may (hopefully) result from a fault breaking and sliding along only one segment of the fault’s entire length. For example, UVU is on the Provo segment (Payson to Pt. of the Mtn.) of the Wasatch fault. SLC is on the Salt Lake Segment (Pt of the Mtn. to about the State Capitol). The ...
Earth`s Crust Test Prep
Earth`s Crust Test Prep

... On the map above, place an X on the map to show the location of the Nazca Plate. Explain why most major earthquakes are found in specific zones instead of being randomly scattered across Earth’s surface. _______________________________________________________________________ ________________________ ...
To get a better understanding of this whole process, I would like you
To get a better understanding of this whole process, I would like you

... 2. Explain the significance of paleomagnetic banding. Paleomagnetic banding shows that at one point, older rock further from the ridge had been formed at the divergent boundary- only way to explain the zebra like banding of alternating magnetic orientation of the sea floor. 3. Explain the process of ...
Chapter 13 - The Theory of Plate Tectonics
Chapter 13 - The Theory of Plate Tectonics

...  Wind, glaciers, and gravity cause erosion.  Chemical processes break down and change rock through reactions.  When the water flow slows or stops, the particles may be deposited as sediment. ...
Chapter 21: Fossils and the Rock Record
Chapter 21: Fossils and the Rock Record

... younger than the schist, because the granite cuts across the schist. In earthquake-prone areas, such as California, and in ancient, mountainous regions, such as the Adirondacks of New York, there are many faults. As you learned in Chapter 20, a fault is a fracture in Earth along which movement takes ...
On the Move
On the Move

... the Earth’s plates are moving because of convection currents in the asthenosphere. This is the reason for the break up of ...
Oceanic plate region
Oceanic plate region

... This movement causes stress on the Earth’s crust! Sometimes, the stress builds and an earthquake occurs. These boundaries push or pull the Earth so much that it causes cracks to form in the crust called faults! You will learn more about faults later on. ...
PLATE TECTONICS - Part II
PLATE TECTONICS - Part II

... 4) Highly explosive volcanic arc eruptions due to high silica and H2O content 5) Subduction causes ocean basins to collapse 6) Subduction initiates the accretion of exotic terranes 7) Subduction is the site of building new continental crust ...
Answer… - ClassNet
Answer… - ClassNet

... What is moisture on the ground? ...
Let`s think about it. If a lithospheric plate moved 5 centimeters per
Let`s think about it. If a lithospheric plate moved 5 centimeters per

... Introduction: We have been talking about plate movement, but exactly how fast are they moving. Scientist estimate the speed of a moving plate ranges from one to ten centimeters each year. On average, that’s about as fast as your fingernails grow! Even when you are walking slowly, you are moving very ...
ES 3209 Unit 3 Aug 22 2011.indd
ES 3209 Unit 3 Aug 22 2011.indd

Geomorphic Processes: Endogenic and Exogenic
Geomorphic Processes: Endogenic and Exogenic

...  Lichens (algae and fungi living as single unit), remove minerals and weaken rock by releasing acids  Burrowing animals can increase weathering. ...
The geologic evolution of Point Lobos
The geologic evolution of Point Lobos

... the northwest relative to the North American Plate. Much of Northern California and the Pacific Northwest lie on a subducting margin. It is no accident that volcanoes in the “Ring of Fire” around the Pacific Ocean lies along the subducting margins” the Andes, Central America, the Pacific Northwest a ...
Inclusions in Sublithospheric Diamonds
Inclusions in Sublithospheric Diamonds

Geology
Geology

Breakthrough the Discontinuity: 21st Century Mohole
Breakthrough the Discontinuity: 21st Century Mohole

moon
moon

... • Six of the planets in our solar system have natural satellites, or moons. Our moon is Earth’s satellite. • The Apollo space program sent six spacecraft to study the moon. Scientists were able to gather data about the moon’s weak gravity and its effect on astronauts, as well as data about the moon’ ...
Lesson 6: Earthquakes Lesson Plan
Lesson 6: Earthquakes Lesson Plan

... seconds there is an earthquake somewhere in the world. Some earthquakes are barely detected while others cause immense damage and loss of life. Where do earthquakes occur? Like volcanoes, earthquakes mostly occur along plate boundaries. As we know the plates are not motionless but move across the ma ...
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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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