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Profile Documents Logout
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Vocabulary
Vocabulary

... Theory that Earth’s crust and mantle are broken into plates that float and move around on a plasticlike layer of the mantle. ...
Plate Tectonics
Plate Tectonics

... • The geological theory by Alfred Wegner that states that Earth’s continents were once ONE large landmass “Pangea” and over time the continents slowly moved apart. • Evidence... ▫ Shape of the Earth’s continents  They look like they fit together like pieces of a puzzle ...
version 3
version 3

The Four Layers
The Four Layers

... of nickel and iron. • As the Earth rotates, the liquid outer core spins, creating the Earth's magnetic field. ...
Crust - wwhsearth
Crust - wwhsearth

... liquid state. The outer core is composed of the melted metals of nickel and iron. • As the Earth rotates, the liquid outer core spins, creating the Earth's magnetic field. ...
Unit 7 Study Guide Answer Key
Unit 7 Study Guide Answer Key

... (think about dragging the wooden block across the sandpaper last year) ...
presentation source
presentation source

... • Atoms or molecules in liquids to cohere, but they are not bound to specific neighboring atoms or molecules, ...
Moving Plates: Restless Earth
Moving Plates: Restless Earth

... In the 1960’s, scientists used new discoveries about the sea floor to develop a theory ...
Geology study guide
Geology study guide

... super contennt pangea ...
Geology- Plate Tectonics (Study Guide) This week, you will create
Geology- Plate Tectonics (Study Guide) This week, you will create

... 1. Draw a diagram to show how convection currents affect the movement of tectonic plates. Use arrows to show direction. Describe how convection currents relate to plate tectonics. 2. Contrast/compare: 1) oceanic crust and continental crust 2) lithosphere and asthenosphere 3) outer core and inner cor ...
The Layers of the Earth PPT
The Layers of the Earth PPT

... liquid. * The outer core is made up of iron and is very dense. ...
Overview of Solar System • The solar system is a disk
Overview of Solar System • The solar system is a disk

... • “Continents” pushed up by tectonic flows in mantle. • Recent lava flows, constant resurfacing. • Crater density Î very young surface – only 800 million yrs old. • Thick CO2 atmosphere • Result of runaway greenhouse effect. • Keeps surface very hot (900F). – Lead, brimstone (sulfer) are molten. • R ...
Final Rev Guide Earthqk Volcanoes Plate Tect
Final Rev Guide Earthqk Volcanoes Plate Tect

... Continental and oceanic lithospheric crust move atop the ___________________. Continental crust is composed of low density, thick _____________ material. Oceanic crust is composed of high density, thin, dark ____________ material. Trenches on the ocean floor are associated with what type of boundary ...
Chapter 2, Section 3
Chapter 2, Section 3

... the entire Earth to average 5.5 g/cm3. This is partly due to the effect of compression. However, it is also partly because the material in Earth’s core is mostly iron. Iron is much more dense than rocks, even when it is not under great pressure. ...
plate tectonics review game!!!!
plate tectonics review game!!!!

Catastrophic Events
Catastrophic Events

...  I understand earthquake waves help scientists to construct hypotheses about the structure of the earth’s interior.  I understand the earth has layers, including a crust, a mantle, and a core; the core is divided into a liquid outer core and a solid inner core.  I understand the crust and rigid p ...
What are Earthquakes
What are Earthquakes

... Let’s make a model! ...
plate tectonics
plate tectonics

... RAIO ACTIVE DECAY – Earth’s internal heat source Earth has been losing heat since it formed, billions of years ago. But it’s producing almost as much heat as it’s losing. The process by which Earth makes heat is called radioactive decay. It involves the disintegration of natural radioactive element ...
Essay Question Outline
Essay Question Outline

... • Oceanic Plate more Dense so slips under Continent Plate less dense creating a trench, volcanoes, island arc • Trench: An underwater canyon indicating a subduction zone and convergent plate boundaries. ...
Crust - Mrs. Bock
Crust - Mrs. Bock

... are caused by the very hot material at the deepest part of the mantle rising, then cooling and sinking again --repeating this cycle over and over. ...
Water Systems on Earth
Water Systems on Earth

... for the water cycle ...
How did plate tectonics emerge on Earth?
How did plate tectonics emerge on Earth?

... The lithosphere1, the Earth's outermost mobile layer, is divided into a small number of rigid plates that move over the asthenosphere, the part of the Earth's mantle located immediately beneath it. This system is responsible for geological phenomena such as earthquakes and volcanic activity. It also ...
Seafloor Spreading
Seafloor Spreading

... • The outer core, a 2,000 km thick layer of iron, nickel, and small quantities of other metals. Lower pressure than the inner core means the metal here is fluid. • Convections cells circulate this molten iron. The Coriolis force also influences the movement of this fluid material. • The flow of iron ...
Chapter 10 Notes Blank
Chapter 10 Notes Blank

... -Appalachian mountains of the USA are similar to mountains found in __________& western Europe -Rocks of South America match those in __________ Main __________ to Wegener’s hypothesis was its inability to provide a __________ for the movement of the continents.  __________ Spreading ...
Short course program: Earth and planetary materials and dynamics
Short course program: Earth and planetary materials and dynamics

... SCW: Structure, composition and bombardment history of the solar system A: Nikitha Susan Saji (STARPLAN, Copenhagen): Isotopic constraints on nucleosynthesis, Solar system composition and accretion Elishevah van Kooten (STARPLAN, Copenhagen): Accretion of Earth and the terrestrial planets Anthony Os ...
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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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