Section 1: The Geosphere
... scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natural agent, such as wind, water, ice or gravity. • Erosion w ...
... scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natural agent, such as wind, water, ice or gravity. • Erosion w ...
Exploring Our World
... Click the Return button in a feature to return to the main presentation. Click the Geography Online button to access online textbook features. Click the Reference Atlas button to access the Interactive Reference Atlas. Click the Exit button or press the Escape key [Esc] to end the chapter slide show ...
... Click the Return button in a feature to return to the main presentation. Click the Geography Online button to access online textbook features. Click the Reference Atlas button to access the Interactive Reference Atlas. Click the Exit button or press the Escape key [Esc] to end the chapter slide show ...
Origin of the Universe
... http://www.enchantedlearning.com/subjects/astronomy/planets/jupiter/moons.shtml ...
... http://www.enchantedlearning.com/subjects/astronomy/planets/jupiter/moons.shtml ...
Export To Acrobat ()
... Prior knowledge writing assignment. Put the following assignment on the board or overhead and give the students about 5 minutes to write their answer. Tell them that you will be grading this assignment based on the clarity of their writing and depth of thought rather than on their understanding of t ...
... Prior knowledge writing assignment. Put the following assignment on the board or overhead and give the students about 5 minutes to write their answer. Tell them that you will be grading this assignment based on the clarity of their writing and depth of thought rather than on their understanding of t ...
chapter 1 - Geoclassroom Home
... the additional carbon dioxide introduced since the Industrial Revolution. Have students discuss the pros and cons of governmental regulations, and/or whether our planet can effectively regulate itself and its systems. 2. Geology, the study of Earth, is generally divided into two broad areas: Physica ...
... the additional carbon dioxide introduced since the Industrial Revolution. Have students discuss the pros and cons of governmental regulations, and/or whether our planet can effectively regulate itself and its systems. 2. Geology, the study of Earth, is generally divided into two broad areas: Physica ...
Layers of the Earth PP
... • Lithosphere- crust and rigid outer layer of mantle (upper mantle) • Asthenosphere- solid rock that flows slowly (like hot asphalt, apart of mantle) • Mesosphere-The strong, lower part of the mantle. • Outer Core- liquid layer • Inner Core- solid, very dense ...
... • Lithosphere- crust and rigid outer layer of mantle (upper mantle) • Asthenosphere- solid rock that flows slowly (like hot asphalt, apart of mantle) • Mesosphere-The strong, lower part of the mantle. • Outer Core- liquid layer • Inner Core- solid, very dense ...
Name___________________________ Date______________
... 6.E.2.2 Explain how crustal plates and ocean basins are formed, move and interact using earthquakes, heat flow and volcanoes to reflect forces within the earth. The earth's plates sit on a dense, hot, somewhat melted layer of the earth. The plates move very slowly, pressing against one another in so ...
... 6.E.2.2 Explain how crustal plates and ocean basins are formed, move and interact using earthquakes, heat flow and volcanoes to reflect forces within the earth. The earth's plates sit on a dense, hot, somewhat melted layer of the earth. The plates move very slowly, pressing against one another in so ...
chapter 1 - Solution Manuals
... Earth is a complex, dynamic planet that has continually evolved since its origin some 4.6 billion years ago. Earth can be viewed as an integrated system of interconnected components that interact and affect one another in various ways. Theories are based on the scientific method and can be tes ...
... Earth is a complex, dynamic planet that has continually evolved since its origin some 4.6 billion years ago. Earth can be viewed as an integrated system of interconnected components that interact and affect one another in various ways. Theories are based on the scientific method and can be tes ...
Chapter 3- The Dynamic Earth
... – When water reaches the land as precipitation it either runs off into a stream or soaks into the ground. – Most water enters the ground – Aquifer- a layer of rock that stores ground water. Recharge zone- surface of the land where water enters the aquifer ...
... – When water reaches the land as precipitation it either runs off into a stream or soaks into the ground. – Most water enters the ground – Aquifer- a layer of rock that stores ground water. Recharge zone- surface of the land where water enters the aquifer ...
Internal Structure of the Earth
... • The outer core is made out of liquid Iron and Nickel • The inner core is a solid layer made out of Iron and Nickel • Both layers make up the majority of the weight of the planet ...
... • The outer core is made out of liquid Iron and Nickel • The inner core is a solid layer made out of Iron and Nickel • Both layers make up the majority of the weight of the planet ...
Anyone who has attended elementary school knows Earth is layered
... each layer. This site can be used to clear up misconceptions about how scientists understand the composition of the layers or as an extension for teaching wave movement. The following link takes you to a page (Step 1) containing images of A View of Earth from Above. Below the image are questions for ...
... each layer. This site can be used to clear up misconceptions about how scientists understand the composition of the layers or as an extension for teaching wave movement. The following link takes you to a page (Step 1) containing images of A View of Earth from Above. Below the image are questions for ...
Science Framework
... rock themselves. As the earths crust changes, these fossils are uncovered. We can study the fossils and find out things about the earth’s history. We might find ancient sea animal fossils out in desert or in the mountains, which show that the oceans and continents were once in different shapes and l ...
... rock themselves. As the earths crust changes, these fossils are uncovered. We can study the fossils and find out things about the earth’s history. We might find ancient sea animal fossils out in desert or in the mountains, which show that the oceans and continents were once in different shapes and l ...
Which of these describes the lithosphere and the
... Theory of Plate Tectonics • Crust rides on top of the plates • Plates ride on top of mantle which is in motion due to convection currents – Convection currents can cause plates to move away from each other or toward each other. ...
... Theory of Plate Tectonics • Crust rides on top of the plates • Plates ride on top of mantle which is in motion due to convection currents – Convection currents can cause plates to move away from each other or toward each other. ...
Volcanoes and Igneous Activity Earth
... • Study of earthquake waves is called seismology • Earthquake recording instrument (seismograph) • Records movement of Earth • Record is called a seismogram ...
... • Study of earthquake waves is called seismology • Earthquake recording instrument (seismograph) • Records movement of Earth • Record is called a seismogram ...
Plate boundary Tour
... As you have learned, where there is upwelling of the asthenosphere, the crust above spreads apart, and new material from below bulges up into ridges. Where there is subsidence of the asthenosphere, the crust is being pulled down along with it to form depressions, or trenches. This can be visualized ...
... As you have learned, where there is upwelling of the asthenosphere, the crust above spreads apart, and new material from below bulges up into ridges. Where there is subsidence of the asthenosphere, the crust is being pulled down along with it to form depressions, or trenches. This can be visualized ...
Name Youngblood, Period
... Plate Tectonics (Read “Continents Adrift” at the first site AND “Plate Tectonics” at the second site. You’ll have to click on “How do we know this?” to get to the information.) 1. Name of the German scientist who first noticed that the coastlines of Africa and South America fit together like puzzle ...
... Plate Tectonics (Read “Continents Adrift” at the first site AND “Plate Tectonics” at the second site. You’ll have to click on “How do we know this?” to get to the information.) 1. Name of the German scientist who first noticed that the coastlines of Africa and South America fit together like puzzle ...
the earth`s interior
... part of the mantle directly below it. This part of the mantle is called the asthenosphere. The consistency of the asthenosphere is like taffy. The asthenosphere is hot, and, like warm taffy, it can flow. The movement of the plates of the lithosphere on top of the slowly moving asthenosphere accounts ...
... part of the mantle directly below it. This part of the mantle is called the asthenosphere. The consistency of the asthenosphere is like taffy. The asthenosphere is hot, and, like warm taffy, it can flow. The movement of the plates of the lithosphere on top of the slowly moving asthenosphere accounts ...
Science Study Guide - Thomas C. Cario Middle School
... Energy released by an earthquake that travels through the earth 10. What is a seismograph? Tool used to measure the amount of energy released by an earthquake 11. Explain how seismic waves tell us about Earth’s interior Speed up in more dense substances and slow down in less dense. P waves can trave ...
... Energy released by an earthquake that travels through the earth 10. What is a seismograph? Tool used to measure the amount of energy released by an earthquake 11. Explain how seismic waves tell us about Earth’s interior Speed up in more dense substances and slow down in less dense. P waves can trave ...
Review: Ring of Fire and Earthquakes
... Two types of land forms occur when plates converge: 1. Subduction Zone ...
... Two types of land forms occur when plates converge: 1. Subduction Zone ...
Historical Geology
... • an instrument that measures the proportions • of atoms with different masses ...
... • an instrument that measures the proportions • of atoms with different masses ...
Earth`s vertical electric field
... The generation and movement of charge through thunderstorms and lightning only occurs over a small part of Earth’s surface. Everywhere else, the air acts like the insulating gap between our parallel plates...almost. Air is a poor conductor but it is not an insulator. Even though its resistance is hi ...
... The generation and movement of charge through thunderstorms and lightning only occurs over a small part of Earth’s surface. Everywhere else, the air acts like the insulating gap between our parallel plates...almost. Air is a poor conductor but it is not an insulator. Even though its resistance is hi ...
Chapter 28 Plate Tectonics Lab
... deep ocean trenches. Some mid-ocean ridges are labeled as rises (i.e., the East Pacific Rise). List one example of each from your map in the second column in the table below. 2. In the third column, list which kind of plate boundary is associated with each feature. The map on the last page of this l ...
... deep ocean trenches. Some mid-ocean ridges are labeled as rises (i.e., the East Pacific Rise). List one example of each from your map in the second column in the table below. 2. In the third column, list which kind of plate boundary is associated with each feature. The map on the last page of this l ...
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.