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Science 4th 9 weeks
Science 4th 9 weeks

...  Major geologic events that occur over eons or brief moments in time continually shape and reshape the surface of the Earth, resulting in continuous global change.  The cosmos is vast and explored well enough for us to know its basic structure and operational principles.  All life is interdepende ...
Layers of the Earth rap
Layers of the Earth rap

... Ready to begin so without further ado I’mma hop up on this fresh beat so I can teach you About the layers of the Earth, first things first The outermost layer is the crust filled with dirt And rocks and sand, I hope you understand The crust is the layer on top of which we stand Its made out of rocks ...
COMPOSITION OF THE EARTH`S MANTLE - IDC
COMPOSITION OF THE EARTH`S MANTLE - IDC

... In this area the resistance friction initiates from the rotation of the solid Earth (some crystalline solids) with the fluid outer core in the same sense generating a lot of tension and heat. ...
PLATE TECTONICS
PLATE TECTONICS

... First thought to be the result of a permanently magnetized core. However, it has been shown that when any substance is heated above 500 degrees C it looses its permanent magnetism. Earth is a Dynamo - Outer core is a fluid consisting largely of iron, so it is an excellent conductor. Electromagnetic ...
A 13-Page Resource of Earth and Space Science Worksheets
A 13-Page Resource of Earth and Space Science Worksheets

... This is a fracture along which the blocks of crust on either side have moved relative to one another parallel to the fracture. This is the outermost major layer of the earth, ranging from about 10 to 65 km in thickness worldwide This is how fast a point on the ground is shaking as a result of an ear ...
Earth & Ocean Formation
Earth & Ocean Formation

... 3. Mesosphere - rigid but not as hard as lithosphere • higher temp than asthenosphere, but not molten because of compression pressure • 4950km thick ...
Geologic Hazards
Geologic Hazards

... • Solid, strong, rigid/brittle outer shell of Earth • Composed of both crust and uppermost mantle • Makes up Earth’s tectonic “plates” – Asthenosphere (extends downward ~100-350 km) • Heat-softened yet solid rock • Plastic (capable of flow) zone on which the lithosphere “floats” ...
Earth`s Layers
Earth`s Layers

... Processes that affect Earth’s surface are often a result of what’s going on inside Earth. But what’s inside Earth? This question is very difficult to answer, because geologists are unable to see deep inside Earth. But geologists have found other methods to study the interior of Earth. Geologists hav ...
Chapter 1 Lecture PowerPoint Handout
Chapter 1 Lecture PowerPoint Handout

... the earthquake. As many as 1000 people were buried under 8 meters (26 feet) of landslide debris. Geologists seek to understand the processes that create such events. (Photo by Reuters/STR/Getty Images Inc.-Hulton Archive Photos) ...
crust, mantle, outer core, inner core
crust, mantle, outer core, inner core

... Appalachian Mountains are a type of these ( fault-block mountains, folded mountains, upwarped mountains) Folded mountains ...
CH 3 - 4
CH 3 - 4

... Magma – liquid melted rock Lava – magma that spills out on the planet’s surface Volcano – the opening in the Earth’s crust through which lava flows Earthquakes – he shock waves or vibrations caused by movement along a fault ...
Factors that Shape the Earth
Factors that Shape the Earth

... crust forms, old crust is forced into trenches along the continents where it is returned to Earth’s mantle and forms magma again. These trenches are called subduction zones. Evidence of sea-floor spreading includes heat measurements, volcanic activity, age measurements, and orientation of magnetic c ...
Integrated Science Chapter 19 Notes Section 1: Earth`s Interior and
Integrated Science Chapter 19 Notes Section 1: Earth`s Interior and

... → In the outer mantle the rocks are mostly solid → The inner mantle is extremely hot and rock is soft and easily deformed ⇒ The core – the center of a planetary body → Composed mainly of iron and nickel → The inner core is solid metal → The outer core, which surround the inner core is liquid metal • ...
Crust
Crust

... 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 ...
Science Review Checklist5
Science Review Checklist5

... 18. The inner core is solid due to the _____ of the other layers. 19. The Earth’s _____ energy within the core moves the mantle ...
Chapter 7
Chapter 7

... • Combines the hypothesis of continental drift with the theory of sea floor spreading. • Earth’s crust and upper mantle broken into plates. • Shift on layer of molten rock. ...
PANGEA
PANGEA

Earth- information sheet Homework T4 Wk1
Earth- information sheet Homework T4 Wk1

... mantle – the layer between the surface of the earth, its crust, and its hot liquid core. The inside of the Earth is active andearthquakes, volcanoes and mountain building takes place along the boundaries of the tectonic plates. As a result of the Earth’s geological activity (the volcanoes and earthq ...
Changes to the Earth`s rocks and atmosphere
Changes to the Earth`s rocks and atmosphere

... The Earth has a layered structure. Large-scale movements of the Earth’s crust can cause changes in the surface rocks. The Earth consists of an inner and outer core, then a mantle and finally a thin crust. The Earth’s crust and the upper part of the mantle are cracked into a number of large pieces ca ...
Chapter 14
Chapter 14

... include metals and fossil fuels, and the distribution of these materials across the earth’s surface is highly variable leading to concentrated deposits in certain areas (e.g., diamonds in Angola or oil in Saudi Arabia). This unequal distribution can lead to conflicts and has implications for nationa ...
No Slide Title
No Slide Title

... were identical…how’dey do dat? Patterns from movement of ice indicate continents were once together ...
ANSWER KEY Name - Riverdale Middle School
ANSWER KEY Name - Riverdale Middle School

... c.) What process is shown occurring at C, and why does it occur? Subduction, because the ocean floor is so much heavier (denser) than the land ...
File - C. Shirley Science EJCHS
File - C. Shirley Science EJCHS

... surface of the crust. The deepest well that has been drilled into Earth’s interior is only about 12 km deep so alternative methods such as seismic waves are used to learn about the interior. Seismic waves are the waves that travel through Earth’s interior during an earthquake. A seismic wave is alte ...
Science 7 Midterm: Study Guide
Science 7 Midterm: Study Guide

... 3. A fossil that is found at a lower level in the ground is ______ than another fossil above it. 4. What type of fossils are made from animal tracks that become fossils when they fill with sediment and eventually turn to rock? 5. The use of rocks and fossils to determine if an object is older or you ...
Geology: The Earth and Its Changes
Geology: The Earth and Its Changes

... Science 5.3.2.a: Analyze and interpret data identifying ways Earth’s surface is constantly changing through a variety of processes and forces such as plate tectonics, erosion, deposition, solar influences, climate, and human activity ...
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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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