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Plate Tectonic Notes
Plate Tectonic Notes

... closest to the crust? • What would be different/happen if the core ...
4 Resources from the Ocean Critical Thinking
4 Resources from the Ocean Critical Thinking

... 3. Some comes from the land. Some is made of the remains of sea creatures that settle to the bottom when the creatures die. 4. Tectonic plates move apart, creating tension. Cracks form in the crust. Melted rock rises through the cracks, cools, and hardens. The hardened rock forms the ridge. ...
1.Using the table above, decide if the element mercury (Hg) should
1.Using the table above, decide if the element mercury (Hg) should

Unit 1
Unit 1

... 4. The earth crust is made up of various rocks. 5. The present development of physical geology has been obtained due to the progress in paleontology. 6. The lithosphere and hydrosphere are covered with a gaseous envelope called atmosphere. 7. The earth’s surface is continually changing. 8. The probl ...
Continental Drift and Plate Tectonics Part 1 Multiple Choice
Continental Drift and Plate Tectonics Part 1 Multiple Choice

... 5. Many early mapmakers thought Earth’s continents had moved based on ____. a. plate boundary locations c. climatic data b. fossil evidence d. matching coastlines ...
1 - Tahoma
1 - Tahoma

... politics obstructed science. South Africa had beaten the British forces in the Boer War, and many South Africans sided with Germany during World War I. Due to these political realities, the theory of continental drift was not taken seriously.. Testable Hypotheses for Plate Motion: Harry Hess The rel ...
Ocean Margins - Penn State York Home Page
Ocean Margins - Penn State York Home Page

... Margins are the submerged outer edge of the continental crust. Consisting of the “shelf “and “slope”. The continental margin extends to where the granitic continental crustal rock stops and the ocean crust basalt begins. This point is associated with the “rise”. ...
Chapter 5 – Volcanos and other igneous activity
Chapter 5 – Volcanos and other igneous activity

... Chapter 5 Volcanos and other igneous activity The nature of volcanic eruptions  Viscosity is a measure of a material’s resistance to flow  Factors affecting viscosity • Temperature - Hotter magmas are less viscous • Composition - Silica (SiO2) content • Higher silica content = higher viscosity (e. ...
oceanic crust - Duluth High School
oceanic crust - Duluth High School

...  Everest is part of the Himalaya mountain range along the border of Nepal and Tibet.  At 9,800 feet, for example, there's about 2/3 of the oxygen in the air than at sea level. At 20,000 ft, there is roughly half the oxygen content in the air. At 29,035ft, the summit of Everest, there is only a thi ...
The Earth`s Layers Foldable
The Earth`s Layers Foldable

Earth!!! - CanScience
Earth!!! - CanScience

... • Heating the lower mantle causes the material to expand. • Since less dense materials float on more dense materials, ...
1 MAY 2011 Oceanogra phy Ch 2 Plate Tectonics and the Ocean
1 MAY 2011 Oceanogra phy Ch 2 Plate Tectonics and the Ocean

... Organisms distribution. Several fossils (Mesosaurus), which can only be explained by drifting continents or a land bridge. ...
Document
Document

... The drift of Europe and Africa away from the Americas C. The collision of two continental plates D. Mid-oceanic ridges E. The conduction currents in the hot magma ...
s-BLOCK ELEMENTS - einstein classes
s-BLOCK ELEMENTS - einstein classes

Geochemistry 303
Geochemistry 303

... What chemical system to use differences between systems Choosing a bulk rock composition ...
Earth Interior Ppt - www .alexandria .k12 .mn .us
Earth Interior Ppt - www .alexandria .k12 .mn .us

... 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 ...
Click here for notes to put into foldable.
Click here for notes to put into foldable.

... The Four Layers (don’t put in 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 grea ...
map-view - Bakersfield College
map-view - Bakersfield College

... Measuring the “strike” of strata • represents the intersection of the tilted layer and the imaginary horizontal plane • A MAP symbol – showing the “directional trend” of strata Measuring the directional ...
i-vi_MCD-SCI-EA-B-FM.indd - Middletown Public Schools
i-vi_MCD-SCI-EA-B-FM.indd - Middletown Public Schools

Document
Document

... Plate Tectonics • New ocean basins form from volcanism • Ocean floor forms IN BETWEEN pieces that have split • SEAFLOOR SPREADING ...
Earth Science, Level 3
Earth Science, Level 3

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 ...
+ CuO Cu + O
+ CuO Cu + O

... Write the scientific term: 1- The arrangement of the metals in a descending order according to the degree of their chemical activity is called ( ……………………………………….) 2- The substance which loses an electron or more during a chemical reaction. (…………………………………………) 3- The substance which takes oxygen away ...
Unit 3 Dynamic Earth
Unit 3 Dynamic Earth

... • An earthquake is the shaking of the Earth’s crust. • The study of earthquakes is called Seismology • The instrument used to measure an earthquakes magnitude (strength) is a seismometer and seismograph ...
Sea Floor Spreading
Sea Floor Spreading

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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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