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Physics 127 Descriptive Astronomy Homework #12 Key (Chapter 6
Physics 127 Descriptive Astronomy Homework #12 Key (Chapter 6

... 6-4. Rocks found on the moon are between 3.1 and 4.47 billion years old. By contrast, the majority of the earth's surface is made of oceanic crust that is less than 200 million years old, and the very oldest earth rocks are about 4 billion years old. If the earth and moon are essentially the same ag ...
Plate Tectonics Review Sheet
Plate Tectonics Review Sheet

... Geologist have used two main types of evidence to learn about Earth’s interior: Rock samples and Seismic waves Seismic waves – When earthquakes occur, they produce seismic waves. Geologists used the data from these waves to learn that the earth interior is made up of several layers Crust – a layer o ...
Plate Tectonics Review Sheet
Plate Tectonics Review Sheet

Directed Reading B
Directed Reading B

... Circle the letter of the best answer for each question. ...
Land, Water, and Air
Land, Water, and Air

... • Includes the crust, mantle, and core • The crust and top layer of mantle are divided into huge, irregular-shaped slabs of rock called plates ...
Unit Test Earth Patterns, Cycles, and Changes Name
Unit Test Earth Patterns, Cycles, and Changes Name

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PPT

... SPI 0707.7.3 Identify the major processes that drive the rock cycle. SPI 0707.7.4 Differentiate among the characteristics of the earth’s three layers. SPI 0707.7.5 Recognize that lithospheric plates on the scale of continents and oceans continually move at rates of centimeters per year. SPI 0707.7.6 ...
Geology of the Inner Planets
Geology of the Inner Planets

... NASA's Mariner 10 spacecraft made its first flyby of Mercury in March 1974, and was also the only Mariner mission to visit two planets (the other was Venus). Images beamed back by the spacecraft from 437 miles above the planet revealed a surface very similar to that of the moon. However, Mariner 10 ...
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Study Guide Answers

... Supercontinent, when all continents were one ...
Chapter_2_Section_2_NOTES
Chapter_2_Section_2_NOTES

... Forces that wear down and __break apart _____ the Earth’s crust. a. Weathering: _the process that breaks rocks down into tiny pieces Caused by: _water, ice, and living things (lichens) Helps create: ___soil ___ b. Erosion: __removal of small pieces of rock by water, ice, and wind. Creates ___new lan ...
GEOL 2312 IGNEOUS AND METAMORPHIC PETROLOGY Lecture
GEOL 2312 IGNEOUS AND METAMORPHIC PETROLOGY Lecture

... “Slab Pull” is thus much more effective than “Ridge Push” But both are poor terms: “slab pull” is really a body force (gravity acting on the entire dense slab.. The old question of whether convection drives plate tectonics or not is also moot: plate tectonics is mantle convection. The core, however, ...
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Study Guide Ch. 1

... first people lived near water ...
Chapter 2: Earth Systems: Processes and
Chapter 2: Earth Systems: Processes and

... o This contrast results from different fluxes of solar radiation reaching Earth’s surface o The atmosphere attempts to “smooth out” this temperature gradient by transferring heat from the equator toward the poles by convection o Earth’s wind patterns result from the effects of atmospheric convection ...
Quiz # 7
Quiz # 7

... Identify the letter of the choice that best completes the statement or answers the question. __E__ 1. According to the theory of plate tectonics, a. the continents are moving but the ocean floor is not, leading to great friction b. the rubbing of the waters of the Earth across its crust is speeding ...
study guide - Hull Lessons
study guide - Hull Lessons

... Earth’s lithosphere is formed by the mantle’s rigid upper part and the crust, which is the top, hard rock layer. Beneath the Earth’s crust lies the mantle, which is partly solid and partly semi-solid. During the 1500’s, geographers who made the first accurate maps noticed that the continents seemed ...
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C1 Topic 7 the earth revision Earth`s Structure (and rocks) 1. List the

... hydrogen for the earth’s early experiment? 23. Why does Miller and Urey’s experiment only provide weak evidence? 24. Miller and Urey’s experiment suggested how ………….. …………….. were formed ...
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Earths Layers

... And what type of crust would you like with your Earth? 6. There are two types of crust ...
Science: Earthquake Vocabulary
Science: Earthquake Vocabulary

... SCIENCE VOCABULARY EARTHQUAKES EARTHQUAKE ...
The Earth`s Interior
The Earth`s Interior

... • S-wave shadow zone: the region on the earth’s surface (at any distance more than 103o from an earthquake epicenter) in which S waves from the earthquake are absent • The S-wave shadow zone seems to indicate that S waves do not travel through the core at all, if this is true, it implies that the co ...
Layers of the Earth
Layers of the Earth

... • It is ___________________________ km thick. • There are ________ types of ___________________. • One is _____________________ (very dense, made of ____________________). • The other is ________________________ (less dense, made of ________________________). The Mantle • The ____________________ is ...
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3 Types of heat transfer 2. Conduction

... •Slab Pull •Ridge Push ...
Landforms
Landforms

... • Four important zones in Earth’s Interior – Core-Center: like a nuclear furnace, divided into inner(solid) and outer core (dense liquid metal) – Mantle- Most of Earth’s mass – Crust- 25 miles thick. Currents carry heat from core through the mantle to the crust ...
NTWS TEK 9 A and B
NTWS TEK 9 A and B

... 12. Of that % which is absorbed, how much is redirected back to space as infrared? 13. Briefly describe each of the processes of the hydrologic cycle:  Evaporation  Condensation  Precipitation  Infiltration  Transpiration  Runoff 14. Where on the Earth do the most perpendicular rays of the Sun ...
Layers of the Earth
Layers of the Earth

... •All life exists in the crust of the Earth. •Approximately 90 different elements are found in the crust, but 5 make up 90% of the crustoxygen, silicon, aluminum, iron, & calcium ...
Plate Tectonics - Faculty Perry, Oklahoma
Plate Tectonics - Faculty Perry, Oklahoma

... Landslides that occur when rocks and soil are mixed with water ...
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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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