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KS3 Russia
KS3 Russia

... Around a quarter of a billion years ago, all of the Earth’s land masses are thought to have been joined together in a single supercontinent named Pangaea. It was during the formation of Pangaea, when Euramerica collided with Kazakhstania that the Ural Mountains first developed. Pangaea later split i ...
Name
Name

... 14.) What happens when two plates release built-up tension? __________________________ 15.) What is the most famous transform plate boundary? ____________________________ Part VI: Click on “Back to the first page of Plate Tectonics” or go to: http://www.pbs.org/wgbh/aso/tryit/tectonics/ 16.) Who fir ...
Name
Name

... B) Jupiter-sized planets eject material into their star C) The higher masses of Jupiter-sized planets tend to produce smaller gravitational forces on stars than Earth-like planets at the same distances to the star D) Jupiter-sized planets produce tremendous amount of radio waves that can be detected ...
Geology - Regional School District 13
Geology - Regional School District 13

... 1. Humans depend on Earth for resources that are limited and are distributed unevenly around the planet. 2. Earth is our home; we depend on its resources that mold civilizations, drive human exploration, and inspire human endeavors that include art, literature, and science. 3. Soil, rocks and minera ...
Plate Tectonics Unit(poster)
Plate Tectonics Unit(poster)

... at the ridge and oldest the farthest away from the ridge *2 Basalt rock was found at the mid-ocean ridge, it comes from Volcanoes and makes the ocean floor of every ocean * 3 Ocean floor was found to be sinking below continents or other crust at the trenches… this process was named subduction ...
Mineral resource
Mineral resource

... Chapter 14 Geology and Nonrenewable Mineral Resources ...
Seasons, Solar Intensity, and Latitude
Seasons, Solar Intensity, and Latitude

... • A community of organisms living all parts of their soil. Describes a complex living system in the soil and how it interacts with the environment, plants, and animals. • See diagram on p. 76 ...
The Precambrian: Hadean, Archean and Proterozoic
The Precambrian: Hadean, Archean and Proterozoic

... acid (HCl), which was the source of the chloride in sea salt (mostly NaCl). • The volatiles were probably released early in the Earth's history, when it melted and segregated into the core, mantle, and crust. This segregation occurred because of differences in density, the crust being the "lightest" ...
DO NOT WRITE ON THIS PAPER Earth`s Layers Key Concepts
DO NOT WRITE ON THIS PAPER Earth`s Layers Key Concepts

... A. the inner core B. the outer core C. the crust D. the mantle 2. Earth has five layers based on physical properties: the inner core, the outer core, the mesosphere, the asthenosphere, and the lithosphere. Which of these layers do the tectonic plates move on top of? A. outer core B. lithosphere C. m ...
Earth`s History Lesson 3: Absolute Dating
Earth`s History Lesson 3: Absolute Dating

... • The radioactive isotope is called the parent isotope, and the stable isotope formed by its breakdown is called the daughter isotope. • Half-life is the time needed for half of a sample of a radioactive element to decay and form daughter isotopes. • After one half-life has passed, one-half of the p ...
Interior of the earth
Interior of the earth

... state of gravitational equilibrium between the earth's lithosphere and asthenosphere such that the tectonic plates "float" at an elevation which depends on their thickness and density. This concept is invoked to explain how different topographic heights can exist at the Earth's surface. When a certa ...
Factsheet: Plate Tectonics
Factsheet: Plate Tectonics

... under the ocean. The type of crust that underlies the continents is called continental crust, while the type found under the oceans is called oceanic crust. The border between two tectonic plates is called a boundary. ...
Flash Cards - tclauset.org
Flash Cards - tclauset.org

... Q3-2: Draw a simplified diagram of Earth’s interior: a.) Indicate where on the diagram you would find aluminum & silicon & iron. b.) Using the following density values (Al-2.7, Si2.3, Fe-7.9, H2O-1.0) to explain why water floats on the earth’s surface. c.) How does the density of the mantle compare ...
Earthquake Waves - davis.k12.ut.us
Earthquake Waves - davis.k12.ut.us

... between the arrival time of the P-waves and S-waves. Think of it like timing the distance of lightning by counting the difference between the arrival of light and sound. ...
Plate Tectonics 1
Plate Tectonics 1

... Supporting Continental Drift? Alfred Wegner came up with the Continental Drift Hypothesis. His 5 pieces of evidence were: 1) Continents seemed to fit together 2) Similar fossils on each continent 3) Rocks matched (age and composition) 4) Glacial evidence – striations (scratches in rocks matched) + d ...
Earthquakes/Mountain Building
Earthquakes/Mountain Building

... Stress –pressure/tension ...
Objectives: Geology and soil
Objectives: Geology and soil

Chapter 5 Review
Chapter 5 Review

... If the statement is true, write true. If it is false, change the underlined word or words to make the statement true. (6)Continental crust is made of rocks such as granite. (7)Slow movements of mantle rock called radiation transfer heat in the mantle. (8)The single landmass that broke apart 250 mill ...
Earth`s Crust in Motion – Study Guide
Earth`s Crust in Motion – Study Guide

... ocean crust—plates located in the ocean; more dense than continental plates magma—molten material comes to the surface during sea floor spreading ocean floor—the closer it is to the mid-ocean ridge, the newer it is subduction—ocean floor sinks beneath a deep ocean trench and back into the mantle lan ...
Pangaea
Pangaea

... The plate tectonics theory came about in the 1960s and 1970s as new information was obtained about the nature of the ocean floor, the distribution of volcanoes and earthquakes, the flow of heat from Earth's interior, and the worldwide distribution of plant and animal fossils. The theory states that ...
Plate Tectonics
Plate Tectonics

... Theory of Plate Tectonics (pg 175) • In the 1960s, scientists combined sea-floor spreading, Earth’s plates, and plate motions into the theory of plate tectonics. • Earth’s plates are in slow, constant motion, driven by convection currents in the mantle. ...
Unit 7 Lesson 1 Forces that Change the Earth
Unit 7 Lesson 1 Forces that Change the Earth

... 8:3 Scientific investigation and reasoning. The student uses critical thinking, scientific reasoning, and problem solving to make informed decisions and knows the contributions of relevant scientists. The student is expected to: 8.3A: In all fields of science, analyze, evaluate, and critique scienti ...
Plate Tectonics Notes
Plate Tectonics Notes

...  less dense than lower layers asthenosphere denser, semi-molten layer of Earth  hot and flowing  plastic-like rock layer of the mantle below the lithosphere  soft layer within the mantle that flows like a very thick liquid convection  circular path of heating current and cooling by temperature ...
Intrusive volcanism * a summary
Intrusive volcanism * a summary

Seafloor Spreading: 100
Seafloor Spreading: 100

...  This is why Wegner’s theory of Continental Drift was not accepted.  What is the “how the continents” were able to move?  Bonus: This is the mechanism for movement of the continents.  What is seafloor spreading and ...
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History of geology



The history of geology is concerned with the development of the natural science of geology. Geology is the scientific study of the origin, history, and structure of the Earth. Throughout the ages geology provides essential theories and data that shape how society conceptualizes the Earth.
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