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Part 2…Plate Tectonics
Part 2…Plate Tectonics

... 7. Scientists eventually concluded that the sea floor was spreading. Describe how this occurs. 8. How did oil drilling exploration confirm the idea of sea floor spreading? 9. What did the sea floor spreading theory suggest about the age of the ocean crust as one moves away from the mid ocean ridge? ...
Document
Document

... as they move through the Earth ...
Lecture 13.
Lecture 13.

... This process explains recent changes in the height of sea-level in coastal areas of eastern and northern Canada and Scandinavia. Some locations in these regions of the world have seen sea-level fall by as much as one meter over the last one hundred years. This fall is caused by isostatic rebound. Bo ...
EarthComm_c2s6_185-197
EarthComm_c2s6_185-197

... much evidence that almost all geologists accept the theory. Much of the evidence that Wegener used to support his hypothesis supports plate tectonics. However, new evidence has emerged. This evidence provided a better explanation for the movement of Earth’s lithosphere. One piece of evidence geologi ...
Mt. Fuji, Japan The Theory of Plate Tectonics Steps in Development
Mt. Fuji, Japan The Theory of Plate Tectonics Steps in Development

... 4. Similar Rock Types Across Ocean Basins Mountains of Northern Hemisphere similar in Greenland, NA, and Europe. Also similar rocks between South America and Africa. ...
plate tectonic study guide
plate tectonic study guide

... Tell about the age of the floor. What is the mid-ocean ridge? Longest chain of underwater Mountains (in the world) in the Atlantic ocean --the ocean floor at the mid-ocean ridge produces new oceanic crust and pushes the old crust farther away for the mid-ocean ridge as the crust moves farther from t ...
File
File

... Volcanoes are usually found where two tectonic plates meet (plate boundaries). Remember some volcanoes can form at a hotspot (away from boundaries). ...
Microsoft Word - APES Chapter 16 Study Guide
Microsoft Word - APES Chapter 16 Study Guide

... • All of a resource will not be used because it is not economically feasible to continue to extract the resource. • Usually, the first deposits of a mineral to be exploited are high-grade deposits. • Depletion time is dependent on rate of use and amount of know reserves. 63. Based upon the answer to ...
Earth Science Exam Review 7
Earth Science Exam Review 7

... forest ecosystems. Above the tree line on mountains, however, the ecosystems change. Few birds are found there. Many factors contribute to the lower number of birds seen above a mountain’s tree line. Which of these factors is abiotic? A limited food B no trees for shelter C.frequent high winds D hig ...
Chapter 20 - "Inside the Earth"
Chapter 20 - "Inside the Earth"

... – If the reflected waves reach the surface, they can be measured by a seismograph. – Wave refraction can also be used to determine properties of the interior of the Earth. • Waves are refracted (bent) when they pass from a layer with higher density to a layer with lower density. ...
Lesson 7.1: Volcanoes and Plate Boundaries
Lesson 7.1: Volcanoes and Plate Boundaries

... • Plate boundaries: Earth’s crust is not one whole piece. It is broken up into different pieces we call “plates.” • These plates—think of egg shells—move in different directions because of heat. • Convergent plates—two plates coming towards each other. • Divergent plates—two plates move away from ea ...
Questions for the fifth quiz
Questions for the fifth quiz

... When did Wegner publish his essay Die Enstehung der Kontinente und die Ozeane? How did explain that the continents moved? How was this explanation received? What happened to Wegner’s reputation for the next 50 years or so? What did the paleomagnetic data suggest had happened to India? Are plate boun ...
Variables Change Earth Study Guide
Variables Change Earth Study Guide

... rocks and make them smooth. Over years, canyons get deeper as rivers flow through them and continue to break rocks down. Ice: Glaciers can grind and scrape rocks and weather them into smaller rocks or sediment. Forces that cause erosion are wind, water, and ice. Wind: Wind can blow sediment or dust ...
SOL Review
SOL Review

... because S-waves could not penetrate the molten layer and P-waves were slowed.  It was determined that the inner core is solid because there is a sudden increase in P-wave activity. The inner core is the most dense layer of the earth ...
Plate Tectonics Part 1
Plate Tectonics Part 1

... to slide past each other. – Strain on plates builds up pressure and energy – Sudden movement of these plates produces burst of energy ...
Plate Tectonics Lab Questions Plate Tectonics Lab Questions
Plate Tectonics Lab Questions Plate Tectonics Lab Questions

... Divergent Plate Boundary Discussion Questions 1. What happened to the frosting between the crackers? 2. What do the graham crackers represent? 3. What does the frosting represent? 4. Name a specific location on the Earth where this kind of boundary activity takes place. 5. What type of feature is pr ...
Oceanic Crust
Oceanic Crust

... mantle, crust) • On the surface of the Earth are tectonic plates that slowly move around the globe • Plates are made of crust and upper mantle ...
Ocean 11 - Course World
Ocean 11 - Course World

... 11. Read the following and answer the questions: Scientific team finds “Lost City” during deep-sea tour of Atlantic Oceanographers patrolling the mid-Atlantic in a miniature research submarine have stumbled onto a spectacular deep-sea garden of hot springs and towering spires they nicknamed the 'Lo ...
Chapter 3 Understanding the `big ideas`: major concepts that
Chapter 3 Understanding the `big ideas`: major concepts that

... subjected to great deformational processes in the past, and knew about the high temperatures of magmas and metamorphic rocks, they didn’t know what had caused these enormous pressures and temperatures. Lots of different ideas were suggested, but none of them seemed to give an answer that could expla ...
B. The Mantle
B. The Mantle

... 3. Rainwater is naturally acidic, having a pH of about 5.5 to 6.5. As it hits the rocks and minerals on the surface of the earth, it is a major source of weathering and erosion of earth materials. As it runs down to the low-lying areas, it accumulates. As the sun evaporates the water, it rises as wa ...
DeltaScience - Delta Education
DeltaScience - Delta Education

... each of which has a distinct composition. The rocky outer layer that covers Earth’s surface is the crust. There are two types of crust. Continental crust contains the huge land masses called continents. Continents contain landforms such as mountains and valleys. Oceanic crust lies beneath the oceans ...
Document
Document

...  C. New rock comes to the Earth's surface ...
The Earth’s Layers - Welcome to Ms. George's Science Class
The Earth’s Layers - Welcome to Ms. George's Science Class

... of the mantle rising, then cooling, sinking again and then heating, rising and repeating the cycle over and over. • When the convection currents flow in the mantle they also move the crust. The crust gets a free ride with these currents. • The movement of the mantle is the reason that the plates of ...
Plate Tectonics - domenicoscience
Plate Tectonics - domenicoscience

... continents are put together. Otherwise, continental ice sheets would have originated from the center of the ocean. ...
ES_14e_Lecture_Ch01
ES_14e_Lecture_Ch01

... – Span of time since Earth’s formation – Earth is 4.6 billion years old – Concept of “recent” is different ...
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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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