Study Guide
... Folding occurs AFTER the layers are formed, it is a result of convergent plate movement. Relative Age: the age of one substance when compared to (relative to ) another (older vs younger, 1st, 2nd, 3rd, etc..) Absolute Age: using the half life of radioactive material to find the exact age of a rock o ...
... Folding occurs AFTER the layers are formed, it is a result of convergent plate movement. Relative Age: the age of one substance when compared to (relative to ) another (older vs younger, 1st, 2nd, 3rd, etc..) Absolute Age: using the half life of radioactive material to find the exact age of a rock o ...
Earth structure
... The crust is made of about twelve plates. These are like big rafts floating on the semi-molten mantle. Convection currents within the mantle cause the plates to move. Although they only move about 2 cm/year this can have huge effects over long periods of time. ...
... The crust is made of about twelve plates. These are like big rafts floating on the semi-molten mantle. Convection currents within the mantle cause the plates to move. Although they only move about 2 cm/year this can have huge effects over long periods of time. ...
The Earth
... Oxygen shields against solar UV radiation O2 provides some shielding, but O3, or ozone, provides most of it Most ozone is located in the ozone layer at an altitude of 25 km Shielding is provided by the absorption of UV photons by oxygen molecules (both O2 and O3) and their resultant dissociation S ...
... Oxygen shields against solar UV radiation O2 provides some shielding, but O3, or ozone, provides most of it Most ozone is located in the ozone layer at an altitude of 25 km Shielding is provided by the absorption of UV photons by oxygen molecules (both O2 and O3) and their resultant dissociation S ...
Homework Due Friday, January 15, 2016 The Plate Tectonic Theory
... discovered mountainous ridges along the bottom of the ocean. These ridges appear to be where two plates have started to move apart, allowing molten rock from the underlying mantle to ooze out and fill the space created by the plates’ movement. Plate tectonic theory has also helped scientists explain ...
... discovered mountainous ridges along the bottom of the ocean. These ridges appear to be where two plates have started to move apart, allowing molten rock from the underlying mantle to ooze out and fill the space created by the plates’ movement. Plate tectonic theory has also helped scientists explain ...
- Webgeol
... Geothermics The transmission of the Earth’s warmth from its deep layers to the surface. By extension, the term geothermics also applies to the use of this energy to heat buildings or produce electricity. Hotspots Zones on the Earth’s surface where volcanic action is regular and long-lasting, due to ...
... Geothermics The transmission of the Earth’s warmth from its deep layers to the surface. By extension, the term geothermics also applies to the use of this energy to heat buildings or produce electricity. Hotspots Zones on the Earth’s surface where volcanic action is regular and long-lasting, due to ...
Five Themes of Geography
... 8. Each half of Earth is called a ____________________. 9. The invisible lines that form eastwest circles around Earth are called lines of _______________ 10. The invisible lines that circle Earth from north to south are called lines of_______________. 11. Why is the study of movement useful to ...
... 8. Each half of Earth is called a ____________________. 9. The invisible lines that form eastwest circles around Earth are called lines of _______________ 10. The invisible lines that circle Earth from north to south are called lines of_______________. 11. Why is the study of movement useful to ...
Plate Tectonics Reading
... the bottom of the ocean. These ridges appear to be where two plates have started to move apart. Molten rock from the underlying mantle oozes out and fills the space that has been created by the plates’ movement. The theory of plate tectonics has also helped scientists explain another amazing Earth l ...
... the bottom of the ocean. These ridges appear to be where two plates have started to move apart. Molten rock from the underlying mantle oozes out and fills the space that has been created by the plates’ movement. The theory of plate tectonics has also helped scientists explain another amazing Earth l ...
7th grade Integrated Science
... Grade Earth Science Core Vocabulary Instructions: This vocabulary sheet is very unique because our vocabulary is unique compared to other science classes. The words will either need to be defined or explained. For example, you can easily look up the definition for hydrosphere (combined mass of water ...
... Grade Earth Science Core Vocabulary Instructions: This vocabulary sheet is very unique because our vocabulary is unique compared to other science classes. The words will either need to be defined or explained. For example, you can easily look up the definition for hydrosphere (combined mass of water ...
Changing Earth`s Surface
... _________________: A force that acts on rock to change its shape or volume. _________________: An area where magma from deep within the mantle melts through the crust above it. _________________: A type of fault where the hanging wall slides downward; caused by tension in the crust. ________________ ...
... _________________: A force that acts on rock to change its shape or volume. _________________: An area where magma from deep within the mantle melts through the crust above it. _________________: A type of fault where the hanging wall slides downward; caused by tension in the crust. ________________ ...
Features of Earth`s Crust, Mantle, and Core
... then put your zipper-lock bag on top. What do the magnetic fields of the two magnets look like now? Draw a picture on your data sheet. ...
... then put your zipper-lock bag on top. What do the magnetic fields of the two magnets look like now? Draw a picture on your data sheet. ...
Plate Tectonics Resource Page - Western Reserve Public Media
... The crust and the upper part of the mantle (which is cooler and more rigid than the lower parts) together make up the lithosphere. The lithosphere is broken into huge rocky slabs called tectonic plates. These plates ride on top of the asthenosphere, a hot, semisolid part of the mantle that lies dire ...
... The crust and the upper part of the mantle (which is cooler and more rigid than the lower parts) together make up the lithosphere. The lithosphere is broken into huge rocky slabs called tectonic plates. These plates ride on top of the asthenosphere, a hot, semisolid part of the mantle that lies dire ...
Powerpoint 1
... Relative dating uses the Law of Superposition to estimate the age of an artifact or fossil. Absolute dating uses the amount of radioactive substances in an artifact or fossil to determines its age more precisely. Discussion? ...
... Relative dating uses the Law of Superposition to estimate the age of an artifact or fossil. Absolute dating uses the amount of radioactive substances in an artifact or fossil to determines its age more precisely. Discussion? ...
Plate Tectonics - Fort Thomas Independent Schools
... Wegener’s hypothesis was that all the continents were once joined together in a single landmass. Continental drift – The idea that the continents slowly moved over Earth’s surface. ...
... Wegener’s hypothesis was that all the continents were once joined together in a single landmass. Continental drift – The idea that the continents slowly moved over Earth’s surface. ...
Earth and Space Science (Volcanoes)
... Earth and Space Science (Volcanoes) Grade 8 Science Grade 8 Science Start Date: November 18, 2013 End Date : November 29, 2013 OH_Academic_Content_Standards - Science (2011) - Grade 8 Strand ESS Earth and Space Science Topic ESS.1 This topic focuses on the physical features of Earth and how they fo ...
... Earth and Space Science (Volcanoes) Grade 8 Science Grade 8 Science Start Date: November 18, 2013 End Date : November 29, 2013 OH_Academic_Content_Standards - Science (2011) - Grade 8 Strand ESS Earth and Space Science Topic ESS.1 This topic focuses on the physical features of Earth and how they fo ...
LAYERS OF THE EARTH
... sediment (basically, bits of different elements) is compacted into rock Chalk and limestone are types of sedimentary rocks ...
... sediment (basically, bits of different elements) is compacted into rock Chalk and limestone are types of sedimentary rocks ...
Earth Layers
... earth's layers and write how the model demonstrates characteristics of these parts. 4. After all 4 models are examined, students should, in pairs or groups, evaluate the strengths and weaknesses of each model and choose which model they think is most appropriate. ...
... earth's layers and write how the model demonstrates characteristics of these parts. 4. After all 4 models are examined, students should, in pairs or groups, evaluate the strengths and weaknesses of each model and choose which model they think is most appropriate. ...
Jeopardy Game (ppt 9 MB)
... the name of the effect of continental drift on the magnetic orientation of magnetite in rocks ...
... the name of the effect of continental drift on the magnetic orientation of magnetite in rocks ...
EARTH SCIENCE - Regional School District 17
... • A layer of gases held close to the Earth by gravity • With the help of the ...
... • A layer of gases held close to the Earth by gravity • With the help of the ...
Chapter 3 Notes
... • The equator is the only line of latitude that is a great circle. • The route along a great circle is the shortest distance between two points on a sphere. As a result, great circles are commonly used in navigation, such as for air and sea routes. Finding Direction • One way to find direction on Ea ...
... • The equator is the only line of latitude that is a great circle. • The route along a great circle is the shortest distance between two points on a sphere. As a result, great circles are commonly used in navigation, such as for air and sea routes. Finding Direction • One way to find direction on Ea ...
Mountain formation - Oxford University Press
... through the Earth’s crust and erupts. The material that erupts falls on the ground and becomes solid. With each future eruption, this material gradually builds into a mountain. ...
... through the Earth’s crust and erupts. The material that erupts falls on the ground and becomes solid. With each future eruption, this material gradually builds into a mountain. ...
Bell Ringer Answers 1-31-11
... ways to make new minerals Because most rocks contain several types of minerals. Nonfoliated; because it would have been changed by heat of lava flows and not by high pressure. ...
... ways to make new minerals Because most rocks contain several types of minerals. Nonfoliated; because it would have been changed by heat of lava flows and not by high pressure. ...
Plate tectonics study guide blank File
... 9. What happens to convection currents when the heat source is removed? 10. What does Wegener’s theory of continental drift state? 11. What is the name of the super continent that existed millions of years ago called? 12. What do we call any trace of an ancient organism preserved in rock? 13. What a ...
... 9. What happens to convection currents when the heat source is removed? 10. What does Wegener’s theory of continental drift state? 11. What is the name of the super continent that existed millions of years ago called? 12. What do we call any trace of an ancient organism preserved in rock? 13. What a ...
geo vocab study guide 1
... Continental Drift – the hypothesis that states that the continents once formed a single landmass, broke up, and drifted to their present locations. (Occurred over millions of years) Earthquake – The word earthquake defines itself fairly well. Most earthquakes take place near the edges of tectonic p ...
... Continental Drift – the hypothesis that states that the continents once formed a single landmass, broke up, and drifted to their present locations. (Occurred over millions of years) Earthquake – The word earthquake defines itself fairly well. Most earthquakes take place near the edges of tectonic p ...
Spherical Earth
The concept of a spherical Earth dates back to around the 6th century BC, when it was mentioned in ancient Greek philosophy, but remained a matter of philosophical speculation until the 3rd century BC, when Hellenistic astronomy established the spherical shape of the earth as a physical given. The paradigm was gradually adopted throughout the Old World during Late Antiquity and the Middle Ages. A practical demonstration of Earth's sphericity was achieved by Ferdinand Magellan and Juan Sebastián Elcano's expedition's circumnavigation (1519−1522).The concept of a spherical Earth displaced earlier beliefs in a flat Earth: In early Mesopotamian mythology, the world was portrayed as a flat disk floating in the ocean and surrounded by a spherical sky, and this forms the premise for early world maps like those of Anaximander and Hecataeus of Miletus. Other speculations on the shape of Earth include a seven-layered ziggurat or cosmic mountain, alluded to in the Avesta and ancient Persian writings (see seven climes).The realization that the figure of the Earth is more accurately described as an ellipsoid dates to the 18th century (Maupertuis).In the early 19th century, the flattening of the earth ellipsoid was determined to be of the order of 1/300 (Delambre, Everest). The modern value as determined by the US DoD World Geodetic System since the 1960s is close to 1/298.25.