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How did seafloor drilling help scientists find the evidence to support the seafloor spreading hypothesis?
people here are stupid , really the answer is not hi
What other evidence was needed to determine the rate of seafloor spreading?
The age of each strip of rock(K12 Science 6th Grade :p )
How is sonar used to see seafloor spreading and the age of the sea floor?
Sonar, or sound navigation and ranging, is used to map the seafloor by emitting sound waves and measuring their return time after bouncing off the ocean floor. This technique helps scientists visualize the topography of the seafloor, revealing features such as mid-ocean ridges where seafloor spreading occurs. By analyzing sediment layers and their thickness in relation to the ridges, researchers can determine the age of the seafloor, with younger sediments closer to the ridge and older sediments further away. This data supports the understanding of plate tectonics and the dynamic processes shaping the Earth's crust.
How did research from the Glomar challenge help scientist support the theory of seaflooding spreading?
From Wikipedia: Starting from August 1968, the Glomar Challenger embarked on a year-long scientific expedition, the Deep Sea Drilling Program, criss-crossing the Mid-Atlantic Ridge between South America and Africa and drilling core samples at specific locations. When the age of the samples was determined by paleontological and isotopic dating studies, this provided conclusive evidence for the seafloor spreading hypothesis, and, consequently, for continental drift.
What did the magnetic strips prove in seafloor spreading?
They proved that the seafloor was spreading.
How did the seafloor drilling help scientist find evidence to support the seafloor-spreading hypothesis?
people here are stupid , really the answer is not hi
How did seafloor drilling scientists find evidence to support the seafloor-spreading hypothesis?
dumb question. don't want to write it all
What methods did scientists use for the seafloor?
Scientists used methods such as sonar mapping, deep-sea drilling, and submersibles to study the seafloor. Sonar mapping involves using sound waves to create detailed maps of the seafloor, while deep-sea drilling allows scientists to collect samples of rocks and sediments from the ocean floor. Submersibles are underwater vehicles that can be used to explore the seafloor up close and collect samples and data.
How did seafloor drilling help scientists find the evidence to support the seafloor spreading hypothesis?
people here are stupid , really the answer is not hi
What is onshore oil?
Onshore oil is a nickname for oil that is obtained through oil drilling that is completely on land, as opposed to offshore oil, which is collected from drilling under the seafloor with floating oil rigs.
What wa needed to determine the rate of the seafloor spreading?
The age of each strip of rock(K12 Science 6th Grade :p )
What other evidence was needed to determine the rate of seafloor spreading?
The age of each strip of rock(K12 Science 6th Grade :p )
What are some sound waves are used to develop a map of the features of the seafloor.?
Sonar (Sound Navigation and Ranging) waves are commonly used to develop maps of the seafloor. These waves are emitted from a source and bounce off the seafloor features, providing information on depth, shape, and composition. By analyzing the sound waves that are reflected back, scientists can create detailed maps of underwater landscapes.
What seafloor is the process by which new crust is created when seafloor moves apart and magma rises?
Seafloor Spreading
Do dogfish live on the seafloor?
Yes, dogfish, which are a type of small shark, typically inhabit the seafloor. They are commonly found in a range of environments, including coastal areas and deeper waters. Dogfish often prefer sandy or muddy substrates where they can hunt for prey and hide from predators.
What is seafloor plains?
large regions of the seafloor that appear flat but are not
How is sonar used to see seafloor spreading and the age of the sea floor?
Sonar, or sound navigation and ranging, is used to map the seafloor by emitting sound waves and measuring their return time after bouncing off the ocean floor. This technique helps scientists visualize the topography of the seafloor, revealing features such as mid-ocean ridges where seafloor spreading occurs. By analyzing sediment layers and their thickness in relation to the ridges, researchers can determine the age of the seafloor, with younger sediments closer to the ridge and older sediments further away. This data supports the understanding of plate tectonics and the dynamic processes shaping the Earth's crust.
