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Intro to Plate Tectoncis
Intro to Plate Tectoncis

... Main Features of Plate Tectonics • Lithosphere – top layer of the Earth made up of the crust and the top part of the mantle. • Asthenosphere – solid but plasticlike layer on which the lithosphere sits. – Movement in this layer actually creates movement in the plates. ...
Key to pre/post test - TSDCurriculum
Key to pre/post test - TSDCurriculum

... Learning Goals: We know what is inside of the earth by information from seismic waves and our knowledge of the properties of materials and explain how models help us illustrate relationships that we cannot measure directly. ...
Sea floor spreading and the effects it has on the world In partnership
Sea floor spreading and the effects it has on the world In partnership

... material from the earth’s interior (mantle) rises to the surface and the cool sea water hardens this material into rock. The divergent plates constantly produces new rock from Earth’s mantle. The seafloor closer to the divergent plate is much newer than seafloor farther away. As the molten rock hard ...
Plate Tectonics plate boundaries Blas
Plate Tectonics plate boundaries Blas

... and under each other and sometimes they move away from each other. Plate Tectonics is the theory that describes the formation, movements and interactions of these plates. ...
Science SOL Review
Science SOL Review

... Living things are made of cells. Cells carry out all life processes. New cells come from existing cells. Cells are too small to be seen with the eye alone. By using a microscope, many parts of a cell can be seen. ...
November 2003
November 2003

... The table below provides information collected at seismic stations A, B, and C for the same earthquake. ...
UNIT 2 Metamorphism and tectonic plates: Metamorphism is a
UNIT 2 Metamorphism and tectonic plates: Metamorphism is a

... Metamorphism and tectonic plates: Metamorphism is a process where the type or distribution of the minerals in rocks changes because of high pressure or very high temperatures. This process is called isochemical because the global chemical composition of the rock essentially remains unchanged. Metamo ...
Plate tectonics - 2 Subduction Zones Transform Faults
Plate tectonics - 2 Subduction Zones Transform Faults

... Stress builds up on fault as plates move Stress exceeds strength of fault Fault suddenly slips in an earthquake Plate boundary moves Fault locks again ...
Plate Tectonics
Plate Tectonics

... • The Earths surface is built of plates. • The theory of plate tectonics states that the Earths outermost layer is fragmented into twelve or more large and small plates that are moving relative to one another as they ride atop a hotter, more mobile material. ...
Chapter 20 - "Inside the Earth"
Chapter 20 - "Inside the Earth"

... – The crust is the thin layer of solid, brittle material that covers the Earth. – There are some differences in the crust depending on where on the surface you are. • The crust under the ocean is much thinner than the crust under the continents. • Seismic waves move faster through the oceanic crust ...
Earth`s Layers
Earth`s Layers

... • This crust is not a solid shell. It is broken up into huge, thick plates that drift on top of the soft, underlying mantle. • It is made of oxygen, silicon, aluminum. ...
As we told you in a recent Instruction, much of the Earth`s
As we told you in a recent Instruction, much of the Earth`s

... and the top layer of its Outer Mantle) is made up of moving masses of rock called tectonic plates (tectonic means moving). There are a dozen or so major plates and several minor ones. Most are both partly oceanic (under oceans) and partly continental (under land). These plates float on the asthenosp ...
Plate Tectonics
Plate Tectonics

... • A transform boundary is when two plates slip past each other, moving in opposite directions. • Earthquakes often happen in areas with transform boundaries. • The San Andreas fault in California is a good example of this type of fault • Tend to have the most earthquakes. • Crust is not created or d ...
Chapter 2
Chapter 2

... Despite radioactive heating, rocky bodies have cooled considerably since their formation, so that their outer layers have stiffened into lithospheres. ...
Difference Between the Lithosphere and
Difference Between the Lithosphere and

... of the earth. If we consider the entire mantle as whole, Asthenosphere comprises just over 6% in volume, but it is very important in tectonic plate movement as because of the liquidity of this layer, the overlying layer called Lithosphere is able to move. What is the difference between Lithosphere a ...
Earth Interior quest
Earth Interior quest

... Earth’s Interior Questions Use the internet or a book if you have to. Remember to site the source of your information. Use Wikipedia if it is your only choice. 1. How far across is the entire Earth? 2. At what depth is the core/ mantle boundary? Does it have a name? 3. What makes up the “Lithosphere ...
Plate Tectonics and Continental Drift
Plate Tectonics and Continental Drift

... was a combination of centrifugal force from Earth’s rotation and gravitation forces that ...
Layers Stations
Layers Stations

... and basalt. If you think about the outer layer of an apple, the Earth’s crust would be compared to that. 1. Do you think this the densest layer or least dense layer? Why? ...
Mineral resource
Mineral resource

... Transform Boundaries • Two plates sliding past each other forms a transform plate boundary. Natural or human-made structures that cross a transform boundary are offset—split into pieces and carried in opposite directions. Rocks that line the boundary are pulverized as the plates grind along, creati ...
Physical and Ecological Processes
Physical and Ecological Processes

... Scientists cannot predict when volcanoes will erupt. People live near volcanoes because volcanic ash is extremely fertile and good for farming. ...
Volcanoes - National Geographic Society
Volcanoes - National Geographic Society

... volcanoes also release gases, ash, and rock. It’s a super hot mix that can be both incredibly destructive and creative. Volcanoes form at the edges of Earth’s tectonic plates. These huge slabs of Earth’s crust travel atop the partly molten mantle, the layer beneath the crust. If you could see the pl ...
Cell Biology Review Game
Cell Biology Review Game

... The Himalaya Mountains are located along a portion of the southern boundary of the Eurasian Plate. At the top of Mt. Everest (29,028 feet) in the Himalaya Mountains, climbers have found fossilized marine shells in the surface bedrock. From this observation, which statement is the best inference abo ...
Document
Document

... Subduction Zones: where ocean plates slide under another plate ...
Physical Process
Physical Process

... Scientists cannot predict when volcanoes will erupt. People live near volcanoes because volcanic ash is extremely fertile and good for farming. ...
Mountain Building
Mountain Building

... Answer these questions before we continue on your check-in sheet 6. What are the three types of plate boundaries? 7. Of those three, which does not result in the destruction or formation of new lithosphere? 8. One of the three types of boundaries has 3 subtypes- what are those subtypes? 9. What are ...
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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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