Solid Earth
... Most scientists believe that convection within Earth’s lower and upper Mantle is the major driving force linked to plate motion. Convection is driven my temperature differences/density differences and gravity. ...
... Most scientists believe that convection within Earth’s lower and upper Mantle is the major driving force linked to plate motion. Convection is driven my temperature differences/density differences and gravity. ...
Earth Science Text Assignments
... 38. Explain how the three types of evidence from molten material supported the theory of sea floor spreading. *Rocks shaped like pillows or like toothpaste squeezed from a tube. These rocks can only be formed when molten material hardens quickly after erupting. *The rocks in the ocean floor contain ...
... 38. Explain how the three types of evidence from molten material supported the theory of sea floor spreading. *Rocks shaped like pillows or like toothpaste squeezed from a tube. These rocks can only be formed when molten material hardens quickly after erupting. *The rocks in the ocean floor contain ...
File - Sturgeon City
... causes the iron an nickel to remain solid. The inner core is the hottest part of the earth at over 5000 degrees C. That is about as hot as the surface of the sun. Plate Tectonics The earth’s solid crust is composed of separate sections (plates) that constantly move on a partially molten layer of upp ...
... causes the iron an nickel to remain solid. The inner core is the hottest part of the earth at over 5000 degrees C. That is about as hot as the surface of the sun. Plate Tectonics The earth’s solid crust is composed of separate sections (plates) that constantly move on a partially molten layer of upp ...
The Earth-Moon System - Academic Computer Center
... surface. • The Highlands were formed after the Moon’s crust cooled. • This surface was constantly being impacted during the early years of the solar system. • Much later, but before the Moon’s interior had cooled, very large impacts broke through the crust. Denser rock flowed into the cracks and fil ...
... surface. • The Highlands were formed after the Moon’s crust cooled. • This surface was constantly being impacted during the early years of the solar system. • Much later, but before the Moon’s interior had cooled, very large impacts broke through the crust. Denser rock flowed into the cracks and fil ...
Layers of Earth Study Guide
... The crust in some tectonic plates is mainly continental. Other plates have only oceanic crust. Still other plates include both continental and oceanic crust. Thick tectonic plates, such as those in which the crust is mainly continental, displace more asthenosphere than do thin plates, such as th ...
... The crust in some tectonic plates is mainly continental. Other plates have only oceanic crust. Still other plates include both continental and oceanic crust. Thick tectonic plates, such as those in which the crust is mainly continental, displace more asthenosphere than do thin plates, such as th ...
Motion and Forces (p. 79-92)
... Earth and Moon, showing their sizes and distance to scale. The yellow bar represents a pulse of light traveling from Earth to Moon (approx. 400,000 km or 250,000 mi) in 1.26 seconds. ...
... Earth and Moon, showing their sizes and distance to scale. The yellow bar represents a pulse of light traveling from Earth to Moon (approx. 400,000 km or 250,000 mi) in 1.26 seconds. ...
E.S. SOL Facts
... 6. The same substance has the same density. 7. As mass increases so does the volume. 8. A hypothesis is a prediction about a problem that can be tested. 9. A variable is a changeable factor in an experiment. 10. An independent variable is something the scientist changes. ...
... 6. The same substance has the same density. 7. As mass increases so does the volume. 8. A hypothesis is a prediction about a problem that can be tested. 9. A variable is a changeable factor in an experiment. 10. An independent variable is something the scientist changes. ...
Document
... Oceanic plate is denser than a continental plate so it subducts under the continental plate. At mid ocean ridges two oceanic plates are moving away from one another so they will not subduct. 19. Identifying Relationships New tectonic material continually forms at divergent boundaries. Tectonic plate ...
... Oceanic plate is denser than a continental plate so it subducts under the continental plate. At mid ocean ridges two oceanic plates are moving away from one another so they will not subduct. 19. Identifying Relationships New tectonic material continually forms at divergent boundaries. Tectonic plate ...
sxES_G6_RNG_ch04-A_070-073.fm
... 16. Circle the letter of each sentence that is true about Earth’s inner core. a. It consists of molten metal. b. It is a thick liquid. c. It is not very dense. d. It is under extreme pressure 17. What creates Earth’s magnetic field? ...
... 16. Circle the letter of each sentence that is true about Earth’s inner core. a. It consists of molten metal. b. It is a thick liquid. c. It is not very dense. d. It is under extreme pressure 17. What creates Earth’s magnetic field? ...
tutorial 2: answer
... 0 / 4 . If l 5C / m , compute E at (0,0, z ) and then evaluate it at: a) The origin. b) z = 5 cm c) z = -5cm ...
... 0 / 4 . If l 5C / m , compute E at (0,0, z ) and then evaluate it at: a) The origin. b) z = 5 cm c) z = -5cm ...
Name
... to form continental glaciers that can exceed 2 kilometers in thickness. Glacial ice has a density of about 0.9 g/cm3, just below that of water, and about 1/3 that of granite. What would be the effect of a 2000 meter thick ice sheet on the continent? What would happen when the ice melted? ...
... to form continental glaciers that can exceed 2 kilometers in thickness. Glacial ice has a density of about 0.9 g/cm3, just below that of water, and about 1/3 that of granite. What would be the effect of a 2000 meter thick ice sheet on the continent? What would happen when the ice melted? ...
Vocabulary Quiz
... Matching: For each section, place the letter on the line which best matches each term with its’ description. Do Not draw lines! If I get confused, then it must be wrong! Part I Continental Drift _______1. Continental Drift ...
... Matching: For each section, place the letter on the line which best matches each term with its’ description. Do Not draw lines! If I get confused, then it must be wrong! Part I Continental Drift _______1. Continental Drift ...
Plate Tectonics - St John Brebeuf
... • Two plates are moving away from each other. • The process renews the ocean floor and widens the giant basins. • In the oceans, magma from deep in the Earth's mantle rises toward the surface and pushes apart two or more plates. Mountains and volcanoes rise along the seam. • On land, giant troughs s ...
... • Two plates are moving away from each other. • The process renews the ocean floor and widens the giant basins. • In the oceans, magma from deep in the Earth's mantle rises toward the surface and pushes apart two or more plates. Mountains and volcanoes rise along the seam. • On land, giant troughs s ...
C:\Users\jmhemzac\Desktop\2016 Fall\121rev1f16.wpd
... Describe the different ways that earth materials respond to applied stress: ductile (elastic or plastic) vs. brittle Describe factors that influence the behavior of materials, and how they affect behavior, including: composition, material strength, environmental conditions (temperature and confining ...
... Describe the different ways that earth materials respond to applied stress: ductile (elastic or plastic) vs. brittle Describe factors that influence the behavior of materials, and how they affect behavior, including: composition, material strength, environmental conditions (temperature and confining ...
Schiehallion experiment
The Schiehallion experiment was an 18th-century experiment to determine the mean density of the Earth. Funded by a grant from the Royal Society, it was conducted in the summer of 1774 around the Scottish mountain of Schiehallion, Perthshire. The experiment involved measuring the tiny deflection of a pendulum due to the gravitational attraction of a nearby mountain. Schiehallion was considered the ideal location after a search for candidate mountains, thanks to its isolation and almost symmetrical shape. One of the triggers for the experiment were anomalies noted during the survey of the Mason–Dixon Line.The experiment had previously been considered, but rejected, by Isaac Newton as a practical demonstration of his theory of gravitation. However, a team of scientists, notably Nevil Maskelyne, the Astronomer Royal, were convinced that the effect would be detectable and undertook to conduct the experiment. The deflection angle depended on the relative densities and volumes of the Earth and the mountain: if the density and volume of Schiehallion could be ascertained, then so could the density of the Earth. Once this was known, then this would in turn yield approximate values for those of the other planets, their moons, and the Sun, previously known only in terms of their relative ratios. As an additional benefit, the concept of contour lines, devised to simplify the process of surveying the mountain, later became a standard technique in cartography.