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KEY for Tectonics Study Guide #1
KEY for Tectonics Study Guide #1

... 15. Tell what the inner and outer cores are made of. Describe the difference between the two layers. ...
Chapter 6, Rocks and Minerals Lesson 2, Earth`s Changing Crust
Chapter 6, Rocks and Minerals Lesson 2, Earth`s Changing Crust

... Convection cells in the mantle flow like a liquid. The mantle is always in motion. It rises and pushes against the bottom of the crust. This movement causes the thin, brittle crust at the surface to break into pieces, or plates. The plates move along Earth’s surface. Earthquakes and the slow motion ...
Volcanoes
Volcanoes

... 3 Transform (strike-slip) boundary - sliding mostly horizontally along faults (such as San Andreas Fault) - adjacent plates (usually microplates) slide past each other. The ocean floor spreading causes a symmetric age distribution of the ocean floor around the midoceanic ridge. The age and sediment ...
Igneous Rock
Igneous Rock

...  Igneous rocks are classified two different ways:  Where they were formed  What they are made from (mineral composition) ...
layers
layers

... • Even the deepest oil wells are only a few kilometers deep, and the diameter of the Earth is 12,756 km. ...
Earths_interior_2013 Page 1
Earths_interior_2013 Page 1

... moving A scientific theory of the origin of species of plants and animal The theory that the universe originated 20 billion years ago ...
Deforming the Earth`s Crust
Deforming the Earth`s Crust

... how much tension is happening at that point. The more tension means the more seafloor spreading, resulting in a higher frequency of earthquakes at a particular mid-ocean ridge. ...
TYPES OF CRUSTAL MATERIAL
TYPES OF CRUSTAL MATERIAL

... is composed of two basic types of crustal material. We refer to these as continental crust and oceanic crust. These types of crust differ in several ways. While both are made mostly of igneous rocks (that is, rocks that solidify from molten material), they have different compositions. Ocean crust is ...
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... The Inner Core • dense ball of solid metal (iron and nickel) • extreme pressure from layers above • 1200 km, from outside edge of inner core to center ...
Michelle Mindick
Michelle Mindick

... the   Earth’s  inner   core  where   its   original  thermal   energy   is   contained.   Much   of   this   thermal   energy  was  derived  from  the  energy  present  during  an  array  of  collisions  that  took  place.  This   series ...
Earth Science 3.4 - Sleeping Dog Studios
Earth Science 3.4 - Sleeping Dog Studios

... kilometers below Earth’s surface and extend into the upper mantle. Most metamorphism occurs in one of two settings ...
Unit1EarthsStructure 104.50KB 2017-03-29 12
Unit1EarthsStructure 104.50KB 2017-03-29 12

... 1.1 Earth Systems – The Earth’s crust is part of a dynamic system. ...
Movements of Earth`s Major Plates PPT
Movements of Earth`s Major Plates PPT

... to_________ _________. drop down Draw a picture pg. 413 • Example: Tetons in Wyoming ...
Earth Systems Standard 3, Objective 2 Title: Earth`s Interior Posters
Earth Systems Standard 3, Objective 2 Title: Earth`s Interior Posters

... Materials: Textbook, butcher paper, construction paper, markers, colored pencils, scissors, glue Prediction: Where is the densest layer of the earth? Where are the hottest and the coolest places in Earth? Procedures: 1. You may work on this project individually or in small groups of 2-3. 2. Read ove ...
Continental Drift - Ms. Mosley
Continental Drift - Ms. Mosley

... Under the plates, there is another layer of rock called the mantle. The mantle has two parts. The first part is a rock layer. The second part is made of super-heated rock. The plates float on this super-heated rock, but they don’t float like rafts float in a swimming pool. The melted rock is very th ...
Minerals and Their Physical Properties
Minerals and Their Physical Properties

... Predictable Mineral Associations ...
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How mountains are made

... • Geologic structures are dynamically-produced patterns or arrangements of rock or sediment that result from, and give information about, forces within the Earth – Produced as rocks change shape and orientation in response to applied stress – Structural geology is the study of the shapes, arrangemen ...
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220 12LectureDetails11

Earth`s Interior Chapter-1 Section-1
Earth`s Interior Chapter-1 Section-1

...  Is a dense ball of solid metal  Extreme pressure squeezes the atoms of iron and nickel into a tight solid that can’t become a ...
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200 300 400 500 100 200 300 400 500 100 200 300 400 500 100

... What is the sun, air movement, the shape of the land and water content. ...
EASTERN ARIZONA COLLEGE Historical Geology
EASTERN ARIZONA COLLEGE Historical Geology

... This course is an introduction to the principles and interpretation of geologic history. It emphasizes the evolution of the earth's lithosphere (crust), atmosphere, and biosphere through geologic time. It includes consideration of the historical aspects of plate tectonics, the geologic development o ...
Essential Questions - Thomas C. Cario Middle School
Essential Questions - Thomas C. Cario Middle School

... Surface waves: Slowest wave and cause the most damage. Only travel on the surface of the Earth. 5. How do scientists know what the inside of the Earth is made of? Describe in detail. (hint: your answer should say something about the “shadow zone”) Scientists use the changes in speed and direction of ...
The Lithosphere… - Mr Vincent Science
The Lithosphere… - Mr Vincent Science

... 1. Why do you think the asthenosphere is described as being plastic in nature? ...
Cornell Chap 2,5 - Santa Rosa Home
Cornell Chap 2,5 - Santa Rosa Home

... 3. How do the 2 laws of thermodynamics affect available energy? 4. How do the 3 types of plate boundaries move? 5. What are the layers of the atmosphere and what occurs in each? Matter ...
volcanoes
volcanoes

... Volcanoes are usually located where tectonic plates meet. This is especially true for the Pacific Ring of Fire, an area around the Pacific Ocean where over 75% of the volcanoes on Earth are found. ...
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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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