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NAME SEAFLOOR SPREADING Chapter 5, Section 4 Underwater mountain ranges are called. Scientists used to map these mid-ocean ridges. Sonar Most mid-ocean ridges are, but a few can be seen. (Ex.) In
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To fill out the name sea-floor spreading chapter, follow these steps:
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Begin by introducing the concept of sea-floor spreading and its significance.
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Provide a brief background on the pioneers who contributed to the discovery of sea-floor spreading, such as Harry Hess.
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Explain the process of sea-floor spreading, including the movement of tectonic plates and the role of mid-ocean ridges.
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Discuss the evidence supporting sea-floor spreading, such as magnetic striping and age dating of rocks.
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Describe the different stages of sea-floor spreading, including the formation of new oceanic crust.
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Highlight the significance of sea-floor spreading in the context of plate tectonics and continental drift.
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Include relevant diagrams or illustrations to aid in understanding.
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Conclude the chapter by summarizing the key points and discussing any ongoing research or future discoveries related to sea-floor spreading.

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The name sea-floor spreading chapter refers to the geological process in which new oceanic crust forms at mid-ocean ridges and gradually moves away from the ridge, creating new sea floor.
This chapter is typically included in research studies, geological surveys, and educational reports focusing on tectonic plate movements and the formation of oceanic crust.
To fill out this chapter, include sections on the definition of sea-floor spreading, the geological evidence supporting it, diagrams of mid-ocean ridges, and case studies or examples.
The purpose is to educate readers about the process of sea-floor spreading, its geological significance, and its role in plate tectonics.
Information such as definitions, key processes, diagrams, mineral composition of new crust, the rate of spreading, and effects on oceanic ecosystems should be reported.
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Relevant keywords

1960 subduction denser oceanic ranges ridges cools geologist molten mid continents

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