Seafloor spreading activity 2026

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  1. Click ‘Get Form’ to open the seafloor spreading activity in the editor.
  2. Begin with SECTION 1-4, where you will review and reinforce your understanding of sea-floor spreading. Use the figure provided to answer questions on a separate sheet of paper.
  3. For question 1, identify and describe the feature labeled A on the ocean floor. Make sure to provide detailed observations based on the figure.
  4. In question 2, explain the process occurring at B and discuss its results. This requires a clear understanding of how molten material interacts with oceanic crust.
  5. Question 3 asks about the fate of old oceanic crust as new material rises. Provide a concise explanation based on geological principles.
  6. For question 4, list three types of evidence that support the concept of ocean floor spreading as indicated by the arrows in the figure.
  7. Finally, address question 5 regarding process C and its significance in relation to mantle dynamics.
  8. Complete the vocabulary section by filling in blanks for questions 6 through 10, ensuring you understand each term's relevance to sea-floor spreading.

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12:43 13:46 Along the ocean floor in a pattern that mimics the shapes of the continental. Coastlines. Number twoMoreAlong the ocean floor in a pattern that mimics the shapes of the continental. Coastlines. Number two the age of the rock of the seafloor increases as you get further away from the mid ocean ridge.
Seafloor spreading occurs at divergent plate boundaries. As tectonic plates slowly move away from each other, heat from the mantles convection currents makes the crust more plastic and less dense. The less-dense material rises, often forming a mountain or elevated area of the seafloor.
Convection currents in the molten mantle cause the plates to slowly move about the Earth a few centimeters each year. Many ocean floor features are a result of the interactions that occur at the edges of these plates. The shifting plates may collide (converge), move away (diverge) or slide past (transform) each other.

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Source: Tectonics Volcanic activity causes the seafloor to spread along oceanic ridges, forming new areas of crust and mantle. After being generated, this new oceanic lithosphere cools down and contracts by up to 3% of its own volume.
East Pacific Rise For most ridges (e.g., the CocosPacific ridge) never approaches 90 and the fastest actual spreading rate today is about 150 km Myr1 along the East Pacific Rise separating the Nazca and Pacific plates. Note. The second plate moves clockwise relative to the first plate. From DeMets et al. Sea Floor Spreading - an overview | ScienceDirect Topics sciencedirect.com topics sea-floor-spread sciencedirect.com topics sea-floor-spread
Seafloor spreading is the mechanism of continental drift. Convection currents above magmatic plumes in Earths mantle pull the solid crust apart, allowing new material to well up and solidify. Driven by magmatic convection, the sea floor spreads until it encounters a continental plate and is forced into the mantle.
Seafloor spreading produces major characteristics of the seafloor - 1) the age of the seafloor is progressively older away from midocean ridges, 2) the elevation of the seafloor is progressively lower away from midocean ridges, 3) the magnetic history of the seafloor bears the striped-pattern of the Earths magnetic
New geographic features can be created through seafloor spreading. The Red Sea, for example, was created as the African plate and the Arabian plate tore away from each other. Today, only the Sinai Peninsula connects the Middle East (Asia) with North Africa.

what are the strengths and weaknesses of this model as a model for demonstrating seafloor spreading