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Chapter 17 Plate Tectonics Notes
Chapter 17 Plate Tectonics Notes

... • Glacial till – deposits of glacial sediment on continents that are now in tropical climates. Also, rocks scratched by glaciers. ...
Continental Drift
Continental Drift

... 2.  How are ocean-floor rocks and sediments evidence of seafloor spreading? 3.  How do magnetic strips support seafloor spreading? 4.  What would Wegener say after seeing this evidence? ...
Earth Structure and Composition Teaching Assessment
Earth Structure and Composition Teaching Assessment

... 2. After the model is completed, students will use the fishing line to cut straight through their model so they can observe the layers. 3. Following this activity they will label the diagram from the instructions they were given and answer the following questions in their notebook (students may use ...
Study Guide Questions – Earth Structure and Plate Tectonics What
Study Guide Questions – Earth Structure and Plate Tectonics What

... continents, but the ocean basins were no older than about 200 million years The expanding field of paleomagnetics showed that the continents had moved independently of each other through time. And paleomagnetics would soon yield critical evidence for seafloor spreading Although the idea of mantle co ...
File
File

... Above subduction zones because of the ocean crust being pushed down and eventually melting. This melted magma finds its way up through fissures (cracks) in the Earth’s surface. Mantle (asthenosphere) ...
plate boundaries
plate boundaries

... The origin of Valles Marineris on Mars — the longest trough system in the solar system — was formed by rifting, strike-slip faulting, and ...
Earth Structure/Composition
Earth Structure/Composition

... What is the difference between Continental Crust and Oceanic Crust? Which is more dense – continental or oceanic crust? Which is thicker, yet more buoyant – continental or oceanic crust? Does the depth of the lithosphere and asthenosphere differ in depth under the continents rather than under the o ...
and at the subduction zones Lesser Antilles Subduction Zone
and at the subduction zones Lesser Antilles Subduction Zone

...  Fossils of the same plants and animals found on both sides of the Atlantic Ocean  Strange grooves cut by ancient glaciers that line up ...
plates - Northside Middle School
plates - Northside Middle School

... The volcanoes get younger from one end to the other. ...
Sea-floor_spreading-1--
Sea-floor_spreading-1--

Earth Science and M.E.A.P
Earth Science and M.E.A.P

... • Standard: Investigate the scientific view of how the Earth’s surface is formed. • Learning Target: I’m learning about Sea Floor Spreading because it will help explain Wegner’s Theory of Continental Drift. ...
Plate Tectonics and Continental Drift
Plate Tectonics and Continental Drift

... 3. What are the forces that drive plate tectonics? 4. What happens at the boundaries between plates? 5. How do the different types of plate boundaries impact the regional geology and geomorphology? 6. How has continental drift affected the positions of the continents over time? ...
Rock Cycle Drama - Georgia Standards
Rock Cycle Drama - Georgia Standards

... 1. Assign the movement roles as follows: Rock: The cycle begins as groups 2 & 3 (the wind and rain) begin to make sounds. These forces create weathering conditions and weaken the rock in the crust. As weathering occurs, two chosen students from the crust will break from the interlocked arms of fello ...
APES Review: Earth Systems and Global Changes
APES Review: Earth Systems and Global Changes

... Plates move toward each other; oceanic plate will subduct Continental-Continental convergence= no subduction; plates will buckle – forms tall, folded ...
Layers of the Earth powerpoint
Layers of the Earth powerpoint

... 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 ...
Intro2-3
Intro2-3

... The energy of colliding plates creates new landforms. When two ocean plates collide, they may form deep valleys on the ocean’s floor. When ocean plates collide with continental plates, mountain ranges are formed. Mountains are also created when two continental plates collide. When plates separate, u ...
Unit 8 ~ Learning Guide Name
Unit 8 ~ Learning Guide Name

... separated by great geographic distance. These organisms couldn't have travelled the long distance between these continents, supporting his theory that they were once joined. Evidence 4: Ice Age Explanation 4: Scientists found identical marks caused by the movement of glaciers along the coasts of Afr ...
Instructions: Earth`s Layers Questions
Instructions: Earth`s Layers Questions

... separated by great geographic distance. These organisms couldn't have travelled the long distance between these continents, supporting his theory that they were once joined. Evidence 4: Ice Age Explanation 4: Scientists found identical marks caused by the movement of glaciers along the coasts of Afr ...
MYSTERIES OF PLANET EARTH
MYSTERIES OF PLANET EARTH

...  General observations about Wave Propagation: ...
Part 2, E
Part 2, E

... The Earth’s solid surface and the oceans get deformed by the gravity of the moon and the sun. Geologists __have__ (1) long wondered whether this can _cause / trigger__ (2) earthquakes, and finally they have an answer. __Besides__ (3) causing ocean tides, the sun and the moon also pull at __the___ (4 ...
8th Grade Science Glossary
8th Grade Science Glossary

... Compound - A substance made up of atoms of two or more different elements joined by chemical bonds Compression - In geology, a reduction in the volume of a substance due to pressure changes; occurs when something is pushed in Condensation - The change of state from a gas to a liquid Conduction - Typ ...
Question Set #2 - elyceum-beta
Question Set #2 - elyceum-beta

... 5) Is a hard-boiled egg a good model of the Earth’s different interior zones? Explain your answer ...
Plate Tectonics Lithosphere broken into plates 3 Types of plate
Plate Tectonics Lithosphere broken into plates 3 Types of plate

... Plate Tectonics Def.: A theory that explains the behavior of the Earth’s lithosphere in terms of several moving plates. ...
Earth as a System
Earth as a System

... beneath the lithosphere; made of mantle rock that flows very slowly, which allows tectonic plates to move on top of it – about 200 km thick ...
First Hour Exam, Fall, 2006
First Hour Exam, Fall, 2006

... c. age of the minerals - those at the top date from earlier in Earth's history, while those at the bottom are forming today. d. their chemical composition - those at the top being non-silicates, while those at the bottom are all silicates. 16. While on vacation hiking in Wyoming, you encountered a l ...
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Geology



Geology (from the Greek γῆ, gē, i.e. ""earth"" and -λoγία, -logia, i.e. ""study of, discourse"") is an earth science comprising the study of solid Earth, the rocks of which it is composed, and the processes by which they change. Geology can also refer generally to the study of the solid features of any celestial body (such as the geology of the Moon or Mars).Geology gives insight into the history of the Earth by providing the primary evidence for plate tectonics, the evolutionary history of life, and past climates. Geology is important for mineral and hydrocarbon exploration and exploitation, evaluating water resources, understanding of natural hazards, the remediation of environmental problems, and for providing insights into past climate change. Geology also plays a role in geotechnical engineering and is a major academic discipline.
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