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Plate Tectonics
Plate Tectonics

... Oceanic Crust: under the oceans; thinner, MORE dense; basaltic rock ...
Chapter 21- Planet Earth
Chapter 21- Planet Earth

... Law of Superposition ...
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... 1) One natural feature that can be used to contradict the contracting Earth model is Earth’s heat flow, where in general the highest heat flow is found at: ...
Script - FOG - City College of San Francisco
Script - FOG - City College of San Francisco

... with Earth’s formation – 4.6 billion years ago. So what? Why is it important that Earth has layers? How does that affect us? First, let’s look closer at the core, which is composed of two parts – the liquid iron outer core, and the solid iron inner core. Both of them are under high pressure and are ...
Plate Tectonics
Plate Tectonics

... a moving electric field. It is a dynamo! Earth’s magnetic field varies over time and it protects us from cosmic radiation ...
Physical Properties of Earth`s Layers
Physical Properties of Earth`s Layers

... can travel through solids and liquids, but S waves cannot travel through liquids. When scientists observed that S waves do not travel through Earth’s core, they realized that the outer core is liquid. ...
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... _______________________________(a volcanic rock rich in iron) with alternating magnetic lines. As rock rose from inside the Earth, the iron in the molten rock would align itself in the Earth’s magnetic field before the rock__________________________. The study of the magnetic record is called ______ ...
The Changing Earth
The Changing Earth

... Cinder-Cone Volcanoes B88 • explosive eruptions where layers of cinders land near central vent ...
CRCT Home Study Guide For Science- Due
CRCT Home Study Guide For Science- Due

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... the exact distance between the satellites and the ground station. Over time, these distances change slightly. By recording the time it takes for the GPS ground stations to move a given distance, scientists can measure the speed at which each tectonic plate moves. What happens when plates separate on ...
Continental Drift
Continental Drift

... provides support to CD theory • During ice ages, glaciers covered large areas of land ...
chapter 17 - the earth`s interior and geophysical properties
chapter 17 - the earth`s interior and geophysical properties

... Velocities at 100 km display a pattern consistent with sea floor spreading: hot under the ridges, cold for the rest of the sea floor and continents. At 300 km, the continents are still cold, indicating very deep roots. Some ridges are hot at 100 km but cold at 300 km, while the reverse is true in ot ...
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... living things in the ocean forms what type of sedimentary rock ...
Planetary interiors and surfaces
Planetary interiors and surfaces

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Earth Layer`s PPT

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Journey to the Center of the Earth
Journey to the Center of the Earth

... source of tremendous magnetism; its poles, located roughly at the ends of Earth’s axis, mark magnetic north and south. Dangerous cosmic rays are deflected by the magnetic field back out into space, and our atmosphere remains robust because of this protection. Although most geophysicists feel confide ...
Chapter 1: Meet Planet Earth
Chapter 1: Meet Planet Earth

...  James Hutton (1726-1797), now known as the father of modern scientific geology, assembled evidence and proposed a counterhypothesis called ...
Earth`s Layers
Earth`s Layers

... Thank you for purchasing this product! If you like what you see, consider leaving feedback. Visit my Website to see more of ...
What in Earth?! Deciphering solid earth structure and processes 1 to
What in Earth?! Deciphering solid earth structure and processes 1 to

... What in Earth?! Deciphering solid earth structure and processes 1 to 10,000 seismic stations at a time Abstract Converted teleseismic waves are a building block for imaging and characterizing structure in the Earth's crust and upper mantle. Isolated in their simplest form, as receiver functions, the ...
GCS Earth Science Unit B Test
GCS Earth Science Unit B Test

... C. The Indian Ocean is the most tectonically active place on Earth D. North America and Europe are moving ...
Geology * Part II - Hatboro
Geology * Part II - Hatboro

... rock beneath Earth’s surface 2. Earthquakes occur because of stress built up in rock. Stress is a force that acts on a rock to change its shape or volume. These stresses cause faults (a break or crack in Earth’s lithosphere (underground) along which the rocks move). There are three types: a. Shearin ...
OCEANIC GEOGRAPHY and the EARTH
OCEANIC GEOGRAPHY and the EARTH

... b. Theory #2: comets with ice constantly bombard Earth and fill up basins with water; this theory is probably wrong because most comets have a different isotope of hydrogen than most of earth’s water 3. ocean surface area (largest to smallest): Pacific, Atlantic, Indian, Arctic a. Antarctic Ocean [S ...
3. The Earth system
3. The Earth system

... Our planet is composed of three complex natural systems (Figs. 1 & 2): (1) the climate system, (2) the plate tectonic system, and (3) the geodynamo system. The first is driven by an external source of heat (i.e. the Sun), whereas the second and the third are driven by an internal source of heat (i.e ...
Flash Cards - tclauset.org
Flash Cards - tclauset.org

... A4-14: Continental crust is thicker at 30km & made mostly of granite. Oceanic crust is thinner at 5km deep, is made of basalt, & is denser. ...
HNRS 228 Astrobiology Chap.4 Geology Bennett et al.
HNRS 228 Astrobiology Chap.4 Geology Bennett et al.

...  The Earth’s crust and a small part of its upper mantle form a rigid layer called the lithosphere.  The lithosphere is divided into huge plates that move about over the plastic layer called the asthenosphere in the upper mantle ...
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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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