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Pangaea Wegener video guide 2016 17
Pangaea Wegener video guide 2016 17

... together like puzzle pieces. He called this massive land mass “Pangaea” meaning all/whole earth. He theorized further that around 250 million years ago these continents drifted apart. His theories needed evidence to support them. Directions: List and describe 3 pieces of evidence below. 1. Evidence: ...
What evidence did Alfred Wagner use to support his theory of
What evidence did Alfred Wagner use to support his theory of

... How old are the rocks off the east coast of North America relative to the rocks right along the mid Atlantic ridge, why do you think this is the case? The age of rocks increases as they move away from the ridge. The youngest rocks are closest to the ridge. ...
Chapter 16
Chapter 16

... hardened magma or lava. Source a many non-fuel mineral resources. ...
NS2-M3C3_-_Earths_Oceanographic_History_Exam
NS2-M3C3_-_Earths_Oceanographic_History_Exam

... NS2-M3C3 - Earth's Oceanographic History (Exam) Answer Key: NS2-M3C3 - Earth's Oceanographic History (Exam) ...
APES Study Guide Name Period
APES Study Guide Name Period

... Chapter 8 – Answer the questions below in complete sentences on separate sheets of paper. ...
File
File

... using patterns of primary (P) and secondary (S) seismic wave arrivals – Clarification: The travel speed of seismic waves is strongly influenced by rock density, state of matter (liquid, solid) and pressure from depth. Changing density causes seismic energy to reflect and change direction incremental ...
Inside the Earth Study Guide The format on tests and quizzes is a
Inside the Earth Study Guide The format on tests and quizzes is a

... 4. What do the particles in each look like? 5. What is the difference between a solid and a plastic solid? 6. What are the 5 physical layers and how are they different in their physical properties? 7. Even though it is the hottest in the center of the earth, why is the inner core solid, while the ou ...
Student Book Activity, p. 89 Student Book Question, p. 92
Student Book Activity, p. 89 Student Book Question, p. 92

... plate boundaries because it is here that the plates move in relation to each other. The plates that make up the earth's crust are moving at different speeds and in different directions. For example, the North American plate and the Pacific plate are sliding past each other along the San Andreas Faul ...
117 Ways to Pass the Earth Science Regents
117 Ways to Pass the Earth Science Regents

... Warm fronts ride up the back of cold air and produce longer periods of steady rain and occur both in front of and behind the advancing front. ...
Introduction to Earth Science
Introduction to Earth Science

... elevation between each contour line. • Geologic Maps are those that also contain information about the type and age of rock formations in the area. ...
Flashcards review for Study Blue
Flashcards review for Study Blue

Article 3
Article 3

... 2. What are the scientists who study the Earth’s interior and surface called? 3. How do geologists know what the inside of the Earth is like? 4. How does temperature and pressure change as you travel inside the Earth? 5. How many layers of the Earth are there? ...
Objectives - cloudfront.net
Objectives - cloudfront.net

... • Remember that tectonic plates move very_______________. Sometimes rocks move along easily with the plates, but they can also jam up against a plate or between two_______________. Over time, stress builds up within the rock at the plates_______________ against each other. ...
Seafloor Spreading
Seafloor Spreading

... In contrast to the youngest or newest seafloor rock found at mid-ocean ridges, the oldest rock is found at or close to trenches. The oldest seafloor rock is “only” about 180 million years old. Many continental rocks are much older than this; the oldest continental rock is over 4 billion years old. T ...
Earth Science Library wk 8.cwk
Earth Science Library wk 8.cwk

... The Ideas of Alfred Wegener In the early 20th century Alfred Wegener took these earlier ideas and made a case that the continents indeed move. He gathered evidence from a variety of areas: ...
rocks and rock- forming processes
rocks and rock- forming processes

... Any rock exposed at the Earth’s surface will undergo deterioration by physical and chemical processes of weathering (see Figure 3.5 on page 54). Physical weathering – Results in disintegration of rocks into smaller rocks or smaller mineral grains. Chemical weathering – Involves reactions between min ...
Chapter 4: Igneous Rocks and Plutons
Chapter 4: Igneous Rocks and Plutons

... Upon completion of this material, the student should understand the following. ...
GEOFLUID PROCESSES IN SUBDUCTION ZONES AND MANTLE
GEOFLUID PROCESSES IN SUBDUCTION ZONES AND MANTLE

... 800oC. The objective of precombustion was to further concentrate Os in the highly-refractory SiC present in the acid residues. Os isotopes were measured by a TIMS (ThermoElectron Triton) at the Carnegie Institution of Washington with negative ionization mode. Results and Discussion: The Japanese isl ...
Plate Tectonics
Plate Tectonics

... destroyed when one plate dives under another  Ocean plates sink down under ...
Plate Tectonics
Plate Tectonics

... a moving electric field. It is a dynamo! Earth’s magnetic field varies over time and it protects us from cosmic radiation ...
Chapter 9 Plate Tectonics
Chapter 9 Plate Tectonics

...  When subducting plates contain continental material, two continents _______________.  This kind of boundary can produce new _______________ ranges, such as the Himalayas.  Transform Fault Boundaries  At a _______________ fault boundary, plates grind past each other without _______________ the l ...
Internal Structure of the Earth and Pangean
Internal Structure of the Earth and Pangean

... waves, each of which travels through materials differently. The P-waves travel through all mediums but move more slowly through liquids, the S-waves do not travel through liquids (they change into other waves), and the surface waves only travel along the surface. By examining the characteristics of ...
NSTA Geology Reading 1 • Plate Tectonics
NSTA Geology Reading 1 • Plate Tectonics

... ‣ If seafloor is moving, then places and continents must also be moving ‣ When new oceanic crust from at mid-ocean ridges, both the older oceanic crust and the continents riding atop the plates move - Convection Cells - Cause of Plate Motion? ‣ An accepted cause for plate motion is the idea that con ...
EssayFinal
EssayFinal

... composition of the core of the Earth. After an Earthquake occurs, two subsurface body Waves known as P and S Waves travel from the focus of the quake throughout the Earth. We can observe that P "Primary" waves are the first to arrive after an Earthquake, these are very fast and are compression waves ...
Geology of British Columbia and Vancouver Island
Geology of British Columbia and Vancouver Island

... of British Columbia Accretion of the Intermontane SuperTerrane and consequent thrusting and folding of existing sedimentary rocks into the Rocky Mountains. Approach of more micro-continents. Subduction related volcanism and intrusive bodies. ...
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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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