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The Continental Drift Theory
The Continental Drift Theory

... Paleomagnetism: Basaltic rocks (igneous) forming at mid­ ocean ridges records and locks in the Earth's polarity as it  ...
Continental Drift and Plate Tectonics
Continental Drift and Plate Tectonics

... Why was the idea of continental drift rejected for more than 40 years? Wegner could not provide the force that caused the continents to move. How could huge solid chunks of land have plowed through the ocean floor??? ...
Gram Cracker Lab ppt
Gram Cracker Lab ppt

... transforming boundaries. An example would be the transforming boundaries in California, they are sliding past each other. ...
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File

... • Magma erupts over the thinner plate • Sometimes magma may pile over on the ocean to form islands ...
baumgardner`s modeling of rapid plate tectonic motion
baumgardner`s modeling of rapid plate tectonic motion

... decreases exponentially with increasing temperature and also in a strongly nonlinear manner with increasing deformation rate, he believes [and recently has demonstrated in numerical calculations] that such decreased viscosity naturally occurs throughout large volumes of the mantle as the runaway pro ...
(a) evaluate heat transfer through Earth`s subsystems by radiation
(a) evaluate heat transfer through Earth`s subsystems by radiation

... Solar energy input dominates the surface processes (wind, weather, climate, ocean circulation, etc.) of the Earth, and because the Earth is a sphere, its input is not uniform across the planet. The concentration of solar energy depends on the angle at which the solar radiation arrives. In equatorial ...
Getting to Know: Volcanoes
Getting to Know: Volcanoes

... Under Earth’s crust, temperatures are very hot. Rock deep within Earth becomes so hot that it changes from a solid to a liquid. Because liquid rock is less dense than solid rock, it collects in a layer just under Earth’s hard surface. The melted rock is called magma. Where there are cracks and holes ...
LAYERS OF THE EARTH MODEL
LAYERS OF THE EARTH MODEL

... To complete this model you must:  Build a scale model of the layers of the Earth’s interior (this means the size of the layers in your project should accurately reflect the size of the different layers in the earth in proportion to each other).  Show the element composition of each layer  Show th ...
Lecture 4
Lecture 4

... How did the presence of Glossopteris fossils support Wegener's idea of continental drift? Why are earthquake foci depths associated with transform plate boundaries fairly shallow? ...
8 A plate tectonics failure: the geological cycle and conservation of
8 A plate tectonics failure: the geological cycle and conservation of

... Cycles have been much used in geology, and there are at least three kinds of cycle, and they are sometimes confused: the rock cycle, the material cycle, and the plate tectonic cycle. Since the days of Hutton who, in 1788, saw «No signs of a beginning and no prospect of an end» the geological cycle, ...
1915 – Alfred Wegener`s Observations - GLG310-
1915 – Alfred Wegener`s Observations - GLG310-

... •age of sea floor increases with distance from ridge Mechanism to explain observations: Harry Hess & Bob Dietz in the early 1960’s proposed: Sea Floor Spreading  ocean ridges are above mantle upwellings, which cause seafloor to spread, like a conveyor belt  magma replaces seafloor as it moves away ...
hazards and threats: earthquakes terms and definitions
hazards and threats: earthquakes terms and definitions

... tsunamis (Japanese interpretation means "huge wave"). These waves travel across the ocean at speeds as great as 960 kilometers per hour (597 miles per hour) and may be 15 meters (49 feet) high or higher by the time they reach the shore. ...
FREE Sample Here
FREE Sample Here

... The principle of uniformitarianism does not include unusual or atypical geologic events such as an ice age or asteroid impact. ...
plate tectonics review
plate tectonics review

... PLATE MOTIONS ...
Topic 12 Student Handout copy
Topic 12 Student Handout copy

... The place on Earth’s surface lying directly above the focus. The interface between Earth’s crust and mantle. The boundary between two colliding plates. The energy waves given off by an earthquake. Major regions of volcanic activity that are usually in the interior of plates away from plate boundarie ...
What forces shape the earth?
What forces shape the earth?

... the diagram above, water evaporates into the atmosphere from the surface of the oceans,other bodies of water, and from plants. The water exists in the atmosphereas vapor. Eventually,the vapor cools,condenses, and falls to earth as precipitation-rain oI snow.The water soaksinto the ground, evaporates ...
8.3 Causes of Plate Movements
8.3 Causes of Plate Movements

... There is large body of evidence that plate tectonics move around. WHY DOES THIS HAPPEN???? ...
Section 1 Earth: A Unique Planet Section 2 Energy in the
Section 1 Earth: A Unique Planet Section 2 Energy in the

... Section 1 Earth: A Unique Planet Section 2 Energy in the Earth System Section 3 Ecology ...
Name
Name

... The Earth’s lithosphere is made of a number of solid pieces , called ____________ which move in relation to each other. These plates are “riding” on a more “plastic molten” layer below. This layer is called the ASTHENOSPHERE. The evidence shows that approximately _______ million years ago, the major ...
Geography
Geography

... This results in both volcanoes and earthquakes, due to land being lost (destroyed). ...
Chapter 2 Study Guide
Chapter 2 Study Guide

... A. Earthquakes result from movement at plate boundaries and faults. 1. Plate boundaries and other places where faults occur may relieve builtup pressure in fits and starts. Each release of energy causes what we know as an ______________________. 2. Damage from earthquakes is generally greatest where ...
Obj. 2.1.1 Layers of the Earth A
Obj. 2.1.1 Layers of the Earth A

... b. tensional stress d. transitional stress 2. Tensional stresses commonly cause which of the following? a. strike-slip faults c. thrust faults b. reverse faults d. normal faults 3. Compressional stresses can result in the formation of ____. a. rift valleys c. thrust faults b. horsts and grabens d. n ...
Geologic Features Identification and Summary Activity
Geologic Features Identification and Summary Activity

... crust. Earthquakes result from the dynamic release of elastic strain energy that radiates seismic waves. Earthquakes typically result from the movement of faults, planar zones of deformation within the Earth's upper crust. The word earthquake is also widely used to indicate the source region itself. ...
Evidence
Evidence

... construc@ve  and  destruc@ve  geological  processes.  North  America,  for  example,  has  gradually  grown  in  size  over   the  past  4  billion  years  through  a  complex  set  of  interac@ons  with  other  con@nents,  including  the ...
Continental Drift
Continental Drift

... several year’s movement is released all at once in an earthquake. There are three main types of plate boundary. • Divergent plate boundaries • Convergent plate boundaries • Transform fault boundaries ...
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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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