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Earth as a planet
Earth as a planet

... igneous or sedimentary rocks altered by high temperatures and/or pressures ...
The Floors of the Oceans
The Floors of the Oceans

... Dr. Gerard Bond will discuss some of his research about climate change based on interpretation of deep-sea sediments. Of particular interest for much of his study are ice-rafted materials collected in the North Atlantic. You can see versions of some of his work in the Core Repository ...
Geology and Nonrenewable Minerals
Geology and Nonrenewable Minerals

... Ecological Restoration of a Mining Site in New Jersey, U.S. ...
Volcano Lab 16-17 File
Volcano Lab 16-17 File

... of rock (Go to the wet side of the lab now!) Igneous rock was once melted and cooled to form a solid. The faster the rock cools, the smaller the crystals in the rock. When rock cools very inside the earth slowly we call it intrusive. The crystals that form grow to large sizes like the granite in our ...
hsess1-5
hsess1-5

... Evaluate evidence of the past and current movements of continental and oceanic crust and the theory of plate tectonics to explain the ages of crustal rocks. [Clarification Statement: Emphasis is on the ability of plate tectonics to explain the ages of crustal rocks. Examples include evidence of the ...
Layers of Earth Comparisons
Layers of Earth Comparisons

... Earth’s layers are compared by: • Temperature • Density – (the thickness or depth of the layer) ...
Plate Tectonics
Plate Tectonics

... Lithosphere- made of crust and upper mantle Asthenosphere- made of “plastic” part of mantle Mesosphere- made of strong part of mantle Outer Core- liquid layer of core Inner Core- solid layer of core ...
Metamorphic Rocks
Metamorphic Rocks

... Hills Appalachian Mountains ...
Sea Floor Spreading
Sea Floor Spreading

... are moving away from each other (diverging) ...
The Theory of Plate Tectonics
The Theory of Plate Tectonics

... Answer the following questions on a separate sheet of paper. 4. Describe what happens when (a) two plates carrying oceanic crust collide, (b) two plates carrying continental crust collide, and (c) a plate carrying oceanic crust collides with a plate carrying continental crust. 5. Explain what force ...
File
File

... • Identify the three main rock groups. • Locate examples of each rock type on a map of Ireland. • Understand the formation & main characteristics of two types of rock from each group. • Answer an essay style exam question, explaining in detail the formation of one rock type. ...
Earth`s Structure and Processes Test 1 1. What are the only things
Earth`s Structure and Processes Test 1 1. What are the only things

... about Earth’s mantle? The mantle is less dense than the crust. The mantle is the same density as the crust. The mantle is denser than the crust. The mantle is the same density as the core. ...
Sc 7 Unit 5 Rocks and Minerals
Sc 7 Unit 5 Rocks and Minerals

... This ExploreLearning Gizmo allows the user to classify virtual rock samples based on their appearance according to the common characteristics of igneous, ...
Plate Tectonics
Plate Tectonics

... Each province has unique physical characteristics resulting from its geologic past. Geologic processes produce characteristic structures and features. The core, mantle, and crust of Earth are dynamic systems, constantly in motion. Earth’s lithosphere is divided into plates that are in motion with re ...
Understand the effect of rock type and climate upon the rate, degree
Understand the effect of rock type and climate upon the rate, degree

... Chemical weathering: a rock is broken down by chemical reactions that change its mineral composition and physical and chemical properties; occurs quickly in warm, moist environments because water is needed for the chemical reactions.  Carbonation: Carbon dioxide in rainwater or moisture in the air ...
Kusky Tim
Kusky Tim

... Phanerozoic times but absent in the Precambrian, but overall, there have been few changes in the style of OPS accretion with time. Komatiites and banded iron formations occur predominantly in Archean orogenic belts, reflecting higher mantle temperatures and less oxic seawater composition, respective ...
Igneous Geology - Earth Science Teachers` Association
Igneous Geology - Earth Science Teachers` Association

... Most of the earth’s surface is cold and the rocks are brittle. However the sun’s energy drives processes which take place on the surface. The combination of geothermal energy and solar energy causes geological changes on the surface and inside the earth. All these processes are linked into each othe ...
No Slide Title - physicalallen
No Slide Title - physicalallen

... • Dietz-new crust formation SFS • Paleomagnetism~ magnetic bands occur in pairs on both sides of plate boundaries (Vine and Matthews) • Younger rocks found closer to spreading centers (s.c.), age increases as distance increases away from s.c. (drillships) ...
Internal Forces Shaping the Earth
Internal Forces Shaping the Earth

... buildings. • Aftershocks are smallerscale quakes that occur after the initial shock. • The Richter scale uses information collected by seismographs to determine the relative strength of an earthquake. ...
Sea Floor Spreading
Sea Floor Spreading

... Subduction is a process where the ocean floor sinks back into the mantle at a deep ocean trench. ...
for true or “F” - University of South Alabama
for true or “F” - University of South Alabama

... 5. (T F) Transform plate boundaries only affect oceanic lithosphere. 6. (T F) A dike is a concordant tabular intrusive igneous body. 7. (T F) An electron possesses a neutral charge. 8. (T F) The Earth's interior, if subdivided into layers by composition, consists of the crust, mantle and core. 9. (T ...
Chapter 1: Meet Planet Earth
Chapter 1: Meet Planet Earth

... lifetime of continental crust.  The most ancient oceanic crust of the ocean basins is only ...
Plate Tectonics Matching
Plate Tectonics Matching

...  continents were joined  similar rocks and fossils on separate continents  similar mountain ranges divergent boundary between two plates boundary that are moving apart convergent two plates move together boundary mid-ocean mountains chains at the bottom ridge of the oceans between continents rift ...
Chemical Inputs and Outputs at Subduction Zones: A
Chemical Inputs and Outputs at Subduction Zones: A

Earth`s Interior (Geosphere)
Earth`s Interior (Geosphere)

... earth, turn to your neighbor again and using academic language describe why the structure of the earth is like an apple. ...
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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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