The Dynamic Crust
... plate moves over it. The intense heat melts its way to, or near, the surface becoming sites of volcanic activity. ...
... plate moves over it. The intense heat melts its way to, or near, the surface becoming sites of volcanic activity. ...
Dynamic Earth WebQuest
... 8. Plate Tectonics Theory has been widely accepted since the ___________’s. It states that Earth’s outer layer or _________________ is broken up into ________________. These plates hold ______________________ and _____________________. They are constantly _________________. 9. Continents over time B ...
... 8. Plate Tectonics Theory has been widely accepted since the ___________’s. It states that Earth’s outer layer or _________________ is broken up into ________________. These plates hold ______________________ and _____________________. They are constantly _________________. 9. Continents over time B ...
OUTDOOR SCIENCE SCHOOL VOC (#1 – Test)
... 23. (Pg 11) VOLCANISM – two mountain building processes in which magma (molten rock) either breaks through the surface (lava) = volcano, OR pushes up the earth’s crust = doming (a) volcanism is one of nature’s “constructive” forces 24. (Pg 11) PRODUCER – an organism, usually a green plant, which pro ...
... 23. (Pg 11) VOLCANISM – two mountain building processes in which magma (molten rock) either breaks through the surface (lava) = volcano, OR pushes up the earth’s crust = doming (a) volcanism is one of nature’s “constructive” forces 24. (Pg 11) PRODUCER – an organism, usually a green plant, which pro ...
1 Course description Geology lab Outcomes
... Water flowing down the mountain, or dislodged rocks or particles, realize this potential as motion. This gradual flattening, erosion, is a powerful force explored (along with others) in Part IV. ...
... Water flowing down the mountain, or dislodged rocks or particles, realize this potential as motion. This gradual flattening, erosion, is a powerful force explored (along with others) in Part IV. ...
Name: Doe Date: May 13, 2015 Directions: 1. Read the following
... begins with the formation of (the, main, does) Earth, its layers and how the (layers, convection, solid) interact with each other. ...
... begins with the formation of (the, main, does) Earth, its layers and how the (layers, convection, solid) interact with each other. ...
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 ...
Earth Science Final Exam Study Guide
... 1. What does the theory of plate tectonics state about the earth? 2. What do magnetic stripes on the ocean floor represent? 3. What are the three types of plate boundaries & what features can be found at each? 4. What is Pangaea? 5. What evidence is used to support the theory of continental drift? 6 ...
... 1. What does the theory of plate tectonics state about the earth? 2. What do magnetic stripes on the ocean floor represent? 3. What are the three types of plate boundaries & what features can be found at each? 4. What is Pangaea? 5. What evidence is used to support the theory of continental drift? 6 ...
Earth-Interior Foldable Notes
... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
PPT - Hss-1.us
... The types of rocks are: • (1) Igneous - Rocks that are formed by first heating the earth's material (elements) to a molten lava state. The when the molten lava cools it forms igneous rocks. Today we can see this happening in association with volcanoes. • (2) Sedimentary rocks are rocks that form wh ...
... The types of rocks are: • (1) Igneous - Rocks that are formed by first heating the earth's material (elements) to a molten lava state. The when the molten lava cools it forms igneous rocks. Today we can see this happening in association with volcanoes. • (2) Sedimentary rocks are rocks that form wh ...
Earth-Interior Foldable Notes
... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
Long term geomagnetic variations and whole
... (1) University of Liverpool, School of Environmental Sciences, Geomagnetism Laboratory, Liverpool, United Kingdom ...
... (1) University of Liverpool, School of Environmental Sciences, Geomagnetism Laboratory, Liverpool, United Kingdom ...
The Dynamic Crust Topic 4 Topic 12 in Review Book
... It is believed that hot spots occur where rising magma stays stationary and the plate moves over it. The intense heat melts its way to, or near, the surface becoming sites of volcanic activity. Because the plates move, a series of volcanic mountains form for miles. Continental Drift The outlines of ...
... It is believed that hot spots occur where rising magma stays stationary and the plate moves over it. The intense heat melts its way to, or near, the surface becoming sites of volcanic activity. Because the plates move, a series of volcanic mountains form for miles. Continental Drift The outlines of ...
Section 2: Rocks and Minerals
... _____________ also causes rocks to weather. Rocks have many cracks. Water fills the cracks in the rocks. When the water freezes, it __________________. The freezing water, or ice, acts like a wedge to break the rock into smaller pieces. __________________ causes weathering, too. Raindrops beat on ro ...
... _____________ also causes rocks to weather. Rocks have many cracks. Water fills the cracks in the rocks. When the water freezes, it __________________. The freezing water, or ice, acts like a wedge to break the rock into smaller pieces. __________________ causes weathering, too. Raindrops beat on ro ...
the layers of the earth - NATSCI-A7
... hence called sial. On the other hand, oceanic crust, which is mainly composed of silica and magnesium, is called sima. ...
... hence called sial. On the other hand, oceanic crust, which is mainly composed of silica and magnesium, is called sima. ...
Inside Edition
... form protoplanets which were molten, at first Dense materials like iron and nickel would tend to sink towards the middle As cooling progressed lighter materials floated to the surface like “scum” and formed the crust This was all completed about 4 billion ...
... form protoplanets which were molten, at first Dense materials like iron and nickel would tend to sink towards the middle As cooling progressed lighter materials floated to the surface like “scum” and formed the crust This was all completed about 4 billion ...
Unit 3 Study Guide
... ridges since they happen in the middle of the ocean floor. Sometimes the lava can cool over the fault and that area becomes a volcano. ...
... ridges since they happen in the middle of the ocean floor. Sometimes the lava can cool over the fault and that area becomes a volcano. ...
Chapter 8 Notes What are Earthquakes? The study of earthquakes
... b. Most earthquakes occur on the edges of tectonic plates. i. Tectonic plates moved around on the mantle- the plastic rock that makes up most of the volume of Earth. ii. Tectonic plates move in different directions and at different speeds. iii. Plates can push toward each other (convergent boundary) ...
... b. Most earthquakes occur on the edges of tectonic plates. i. Tectonic plates moved around on the mantle- the plastic rock that makes up most of the volume of Earth. ii. Tectonic plates move in different directions and at different speeds. iii. Plates can push toward each other (convergent boundary) ...
Global Energy Balance
... down. How is a balance achieved? Emission of energy depends on the temperature of the earth ...
... down. How is a balance achieved? Emission of energy depends on the temperature of the earth ...
Name:______________________________ o ___________________ Samples
... Tall ___________________ ridges hidden under the oceans o ___________________ around the world In a few places the ridge or mountain is ___________________ the surface of the ocean Example: ___________________ Mapped using ___________________ o Sonar is a device that ___________________ soun ...
... Tall ___________________ ridges hidden under the oceans o ___________________ around the world In a few places the ridge or mountain is ___________________ the surface of the ocean Example: ___________________ Mapped using ___________________ o Sonar is a device that ___________________ soun ...
Layers of the Earth - Endeavor Charter School
... It is hot as a result of the heat left over from the formation of the planet. Also, the interior is further heated from the release of energy from radioactive substances inside the earth. ...
... It is hot as a result of the heat left over from the formation of the planet. Also, the interior is further heated from the release of energy from radioactive substances inside the earth. ...
Google Earth Plate Boundaries Activity Materials
... 2. Fly to the first stop on the ʻPlate Boundary Tourist Tourʼ listed below. You can get there by typing in the latitude and longitude, or many times by typing in the name of the feature. The teacher may wish to have student volunteers be the ʻtour guideʼ at each stop to keep students engaged. At eac ...
... 2. Fly to the first stop on the ʻPlate Boundary Tourist Tourʼ listed below. You can get there by typing in the latitude and longitude, or many times by typing in the name of the feature. The teacher may wish to have student volunteers be the ʻtour guideʼ at each stop to keep students engaged. At eac ...
Lecture Exam 1
... b. hot spots and shield volcanoes. c. deep ocean trenches and linear mountain belts. d. a mid-ocean ridge that circles the globe. _____ An example of a divergent boundary where continental rifting occurs is: a. the Indian-Eurasian plate boundary and Himalayas b. the African rift valley and Red Sea c ...
... b. hot spots and shield volcanoes. c. deep ocean trenches and linear mountain belts. d. a mid-ocean ridge that circles the globe. _____ An example of a divergent boundary where continental rifting occurs is: a. the Indian-Eurasian plate boundary and Himalayas b. the African rift valley and Red Sea c ...
PlateTectonics PREtest 1. List the 3 main layers of the Earth. What
... what the earth’s layers are made of (what elements) OR Watch Brainpop: Earth’s Structure, then take the quiz (print the results or write the correct answers on the back of this sheet). ...
... what the earth’s layers are made of (what elements) OR Watch Brainpop: Earth’s Structure, then take the quiz (print the results or write the correct answers on the back of this sheet). ...
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.