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This virtual lab explores the concept of plate tectonics, which describes and explains the major features of the earth's surface and how they form and deform over time. The lab includes animations and interactive elements that allow users to visualize the processes of seafloor spreading and subduction, which are the essential processes of plate tectonics. Users can also learn about how scientists use sonar technology to map the shape of the seafloor and study its characteristics, such as the age and elevation of the seafloor, as well as the magnetic history of the earth. The lab provides a comprehensive understanding of the dynamic nature of the earth's surface and the forces that shape it, making it a valuable resource for students and educators interested in geology, geophysics, and earth science.
Typology: Summaries
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Continental Drift and Plate Tectonics Virtual Lab http://earthguide.ucsd.edu/eoc/teachers/t_tectonics/t_tectonics.html
Directions: Click on the box shown to the left, then use that page to fill in the information to the right.
Click forward to 0.05 mybp. What is the main difference you see on the map from 0.05 mybp to present day?
Click on one of the larger color versions of the map. Notice the lighter areas, showing the underwater mountain ranges (mid-ocean ridges) of Earth.
The Basics
Sonar Basics Sonar works by measuring the time it takes for sound to _____________________ off of a surface like the sea floor and return as an echo. The longer it takes for an echo to return, the farther ___________________ the reflective surface, whether it’s the far wall of a canyon or the sea floor.
The Actual Depth Sound waves travel at about __________ meters per second in seawater, so a _____ second round trip covers ~6,000 meters. However, the actual water depth is only half of that- 3,000 meters, because 4 seconds represents ________________ the one way distance to the sea floor.
What do you do with sonar data? After all the data are collected, processed, and _________________, scientists can now visualize the ________________________.
p. 114^ Feel free to click through the other tabs to learn more about different types of sonar technology.
What the Earth looked like in the distance past
Plate Tectonics
Imaging the shape of the sea floor
form
Seafloor spreading Subduction
echolocation
The main differences were that Oceana was farther south, Europe and Asia were more separated into continents and larger islands, and North America was much larger and more connected with Central and South America.
bounce
it takes for
330 330
Key Points A) Seafloor spreading takes place at mid-ocean ridges and produces ______________________, the rock that makes up oceanic crust.
B) The _______________________________ Ridge and East ________________________ Rise are examples of mid-ocean ridges.
C) Mid-ocean ridges reach a typical summit of __________ meters below sea level. D) Seafloor spreading produces major characteristics of the seafloor:
The age of the seafloor is progressively ____________________ away from mid-ocean ridges.
The elevation of the seafloor is progressively lower away from mid-ocean ridges.
The magnetic history of the seafloor bears the ____________________ pattern of the Earth’s magnetic reversals.
_________________________ parts of the seafloor have the greatest potential to have accumulated sediments over the longest time.
Key Points A) Subduction is a geological process in which the edge of a lithospheric plate slides ______________________ the edge of an adjacent plate.
B) Trenches, accretionary wedges (prisms), and volcanic or _________________ arcs are key surface features produced by subduction.
C) A subduction zone is the entire ________________ of subduction between the trench and the volcanic arc.
D) The __________________________ marks the line where subduction begins.
E) What is an accretionary wedge?
p. 115
Seafloor spreading (Key Process #1)
Subduction (Key Process #2)
The plates are moving apart very gradually.
basalt
Mid-Atlantic Pacific
2,
older
striped-
Older
underneath island
area
trench
Accretionary wedges are prisms.