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Magnetic Stripes, Drilling Samples, and Molten Material.
molten material and drilling samples
Pieces of evidence for sea floor spreading include the presence of mid-ocean ridges where new crust is formed, symmetric magnetic striping on either side of mid-ocean ridges, age dating of oceanic crust that shows it gets older as it moves away from ridges, and the discovery of pillow basalts and other volcanic rocks on the ocean floor.
Magnetic stripes on the ocean floor recorded by magnetometers demonstrate alternating patterns of normal and reversed magnetic polarity, supporting the concept of seafloor spreading. The presence of mid-ocean ridges, where new oceanic crust is formed through volcanic activity, provides direct evidence for seafloor spreading. Analysis of rock samples collected from the ocean floor that show progressively younger ages of rocks as distance from the mid-ocean ridge increases supports the theory of seafloor spreading.
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
The three are different. The first is Molten Material,which is indeed erupting along mid-ocean ridges. The scientists dived to the ocean floor in Alvin, a small sumbarine. Alvin was built to withstand the crushing pressures four kilometers down in the ocean. A ridge's central valley, Alvin's crew found strange rocks shaped like pillows. Other rocks looked like toothpaste squeezed from a tube. Such rocks form only when molten material hardens quickly under again and again along the mid-ocean ridges.The second is Magnetic Stripes, which are patterns of the ocean floor that provided more support for sea-floor spreading. Earth's magnetic poles have reversed themselves many times during Earth's history. The last reversal happened 780,000 years ago.The third and final one is Drilling Samples, which came from rock samples obtained by drilling into the ocean floor. The Glomar Challenger, a drilling ship built in 1968, gathered the samples. The Glomar Challenger sent drilling pipes through water six kilometers deep to drill holes in the ocean floor. This feat has been compared to digging a hole into the sidewalk from the top of the Empire State Building.Information from: California Earth Science Textbook, pages 152-153.Hope this helps! ☺-SmallvilleGrl
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
Not really but sea floor sediments thickness increase with increased distance from spreading centers which is good evidence. Other evidence such as magnetic reversals, temperature, dating methods provide the best evidence of seafloor spreading
Scientists discovered that the rocks that were found farther away from the ridge the sample was taken from, the older the rocks were. The most recent rocks were always in the center of the ridges. This showed that sea-floor spreading really has taken place.
Ocean drilling provides evidence for plate tectonics through the study of rock samples retrieved from the ocean floor. By analyzing the age and composition of these rocks, scientists can identify patterns of seafloor spreading and subduction, supporting the theory of plate tectonics. Additionally, the presence of magnetic striping on the ocean floor provides further evidence for the movement of tectonic plates over time. Overall, ocean drilling plays a crucial role in understanding the dynamic processes of the Earth's lithosphere and the movement of tectonic plates.
Magnetic striping: Patterns of alternating magnetic polarity in the rock of the ocean floor provide evidence of the seafloor moving away from mid-ocean ridges. Age of the oceanic crust: Younger rocks are found nearer to mid-ocean ridges, supporting the idea of continuous seafloor creation. Ocean drilling samples: Rock samples from the ocean floor show consistent patterns of increasing age with distance from mid-ocean ridges, supporting the theory of seafloor spreading.
Magnetic striping: alternating patterns of magnetic polarity on the ocean floor. Age of the oceanic crust: younger rocks near the mid-ocean ridges and older rocks farther away. Mid-ocean ridges: underwater mountain ranges with high heat flow and seismic activity, where new crust is formed.