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Chapter 1 – Introducing Earth Study Guide
Chapter 1 – Introducing Earth Study Guide

Earth`s Surface:
Earth`s Surface:

... These upwelling plumes of rock are generated by heat within the Earth’s core, which drives convection cells in the mantle. Plate tectonics is the term used for the study of surface motions on the Earth. “Plates” are pieces of crust, on which the continents and oceans basins reside. Earth’s crust is ...
Earth`s Interior Worksheet A Journey to the Center of the Earth (p. 9
Earth`s Interior Worksheet A Journey to the Center of the Earth (p. 9

... 11. How deep is the mantle? Core (p. 11) 12. The earth’s core is made of two parts… what are they? 13. Which two metals make up both parts of the core (the reason why the core is considered one layer)? Exploring Earth’s Interior (p. 13) Label the layers of the Earth on the drawing below with the wor ...
ppt
ppt

... cool, they lock in their current magnetic field direction. • If they are moved from their point of origin, their internal magnetic signal shows it • The continents DEFINITELY moved! ...
Earth Geology
Earth Geology

... cool, they lock in their current magnetic field direction. •  If they are moved from their point of origin, their internal magnetic signal shows it •  The continents DEFINITELY moved! ...
astron_ch_7c (1)
astron_ch_7c (1)

... the Earth that undergoes tectonic activity. It is made up of the crust and a small part of the upper mantle. ...
Earth`s Interior
Earth`s Interior

... minerals (also magnesium, silicon) 3.  surrounded by crust of relatively light silicon-rich minerals. (You are here.) Earth is differentiated. ...
Earth`s Moving Plates
Earth`s Moving Plates

... and ocean floor spreading and explains how the earth has evolved over time.  Explains the formation, movement, collisions and destruction of the Earth’s crust. ...
Inside Earth Worksheet
Inside Earth Worksheet

... 1. Draw and label a model of the Earth’s layers. Be sure to label both the compositional layers and physical properties layers. You may draw two separate models for each “type” of layers or just one. ...
Slide 1
Slide 1

... 22.1 Earth’s Structure • Scientists can’t see into Earth • We can listen (earthquakes as sound waves) • Or, 12 km holes (about 8 miles) can be drilled for use in analysis ...
Earth`s Structure Vocabulary
Earth`s Structure Vocabulary

... Why did the scientific community reject Wegener’s hypothesis? East African Rift is an example of what? The youngest part of the ocean floor is found close to or far from ocean ridges? According to Continental Drift, how quickly or slowly do continents move? Where can one see the result of plate move ...
Spheres glossary quiz - HSIE Teachers
Spheres glossary quiz - HSIE Teachers

... Terrestrial radiation, conduction, convection currents and the transfer of latent heat via condensation are the ways in which heat is transferred to the atmosphere from the earth’s surface. ...
Quiz # 8
Quiz # 8

... C) the crust appears to be thinner and weaker, and cannot support the creation and motion of solid plates. D) mantle convection appears to be more vigorous and has broken the lithosphere into a multitude of small plates instead of a few large ones. ...
earth interior - Red Hook Central Schools
earth interior - Red Hook Central Schools

... • Produce energy waves called seismic waves that travel through the Earth • Seismologists use these waves to investigate the internal structure of the Earth, like a doctor uses x-rays to investigate the internal structure of a person ...
Snicker`s Science - The Science Spot
Snicker`s Science - The Science Spot

... Cracks in the Earth’s surface along which rocks move are called faults. The Earth’s crust is divided in large pieces called plates. ...
Earth`s Interior
Earth`s Interior

... The outermost layer of solid rock including dry land and the ocean floor. Thickest under mountains, thinnest in the oceans.  Oceanic crust-darker in color and made of basalt.  Continental (land) crust-lighter in color and made of ...
GLOBAL PLATE TECTONICS AND GEODYNAMICS
GLOBAL PLATE TECTONICS AND GEODYNAMICS

... LARGE SCALE GEODYNAMICS ...
Document
Document

... A.Earth is divided into ___________ layers- the crust, mantle, and core. 1. Earth’s layers are arranged by their ___________________________ III. The Crust A.Crust- Earth’s outer layer. Also the _____________________________ layer 1. Solid rock that includes dry land and ocean floor. ...
Plate Tectonics Crossword
Plate Tectonics Crossword

... 4. ______________ zones. Places where the seafloor is forced under continental plates. 5. Section of the Earth below the crust. 7. Paleontologists noticed that these were the same on different continents even though the continents were separated by oceans. 9. Source of heat in the mantle. 11. Seaflo ...
YEAR 7 SCIENCE HOMEWORK /YOU ARE A SCIENTIST 1
YEAR 7 SCIENCE HOMEWORK /YOU ARE A SCIENTIST 1

...  COMPREHENSION: Read and answer the questions below. Read and answer the questions below in single complete sentences  The lithosphere is the outside layer of the Earth. It consists of pieces of crust, called plates, which move very slowly over the surface of the Earth. The lithosphere is made of ...
Bell Activity #11
Bell Activity #11

... A Tectonic Plate Close-up Many tectonic plates not only consist of the upper part of the mantle but also consist of both oceanic crust and continental crust. ...
Earth
Earth

... closest to Moon has slightly stronger pull to Moon => bulges towards it. Other side has weaker pull => bulges away compared to rest of Earth. The Earth spins once a day while the bulge always points towards and away from the Moon => high and low tides. ...
Plate Tectonics Crossword - Science
Plate Tectonics Crossword - Science

... Name: __________________________ ...
Plate Tectonics Crossword
Plate Tectonics Crossword

... Name: __________________________ ...
plate tectonics crossword
plate tectonics crossword

... Name: __________________________ ...
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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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