Rocks that are found at on the sea floor of the Earth differ in magnetizations. Using paleomagnetism, these rocks were known to have preserved an imprint of the changes in the earths magnetism over long periods of geological time, which proved the theory of sea floor spreading.
Ocean floor is primarily created at mid-ocean ridges where tectonic plates move apart, allowing magma to rise from the mantle and solidify as new oceanic crust. This process, known as seafloor spreading, results in the formation of new crust that eventually spreads away from the ridge and contributes to the growth of the ocean floor.
Yes, many species of squids are known to live near the floor of the ocean, where they can find protection and shelter in dens or burrows. These dens provide a safe place for squids to rest and hide from predators.
The age of the sea floor varies, with the youngest being less than 200,000 years old and the oldest being over 200 million years old. This variation is due to the process of seafloor spreading at mid-ocean ridges and the subduction of older seafloor at deep-sea trenches.
The dog laid on the floor.
across the floor.
Granitic strips in the ocean floor ... Novanet
Tools such as sonar mapping, geologic sampling, and paleomagnetism studies were used to provide evidence for seafloor spreading. Sonar mapping allowed for the creation of detailed maps of the ocean floor, revealing features such as mid-ocean ridges and deep-sea trenches. Geologic sampling involved collecting rock samples from the ocean floor to study their age and composition. Paleomagnetism studies focused on analyzing the alignment of magnetic minerals in rocks, providing evidence of past changes in Earth's magnetic field that support the idea of seafloor spreading.
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
the theory of sea-floor spreading
Because of the stripes at the sea floor which are magnetic minerals
Three types of evidence supporting the idea of seafloor spreading include magnetic striping of the ocean floor (paleomagnetism), the presence of young volcanic activity near mid-ocean ridges, and the discovery of deep-sea hydrothermal vents that release hot mineral-rich water. These pieces of evidence suggest that new oceanic crust is continuously forming at mid-ocean ridges and spreading outward.
New material is added to the sea floor when sea floor spreading occurs. When the iron cools it is magnetized by the magnetic field of the earth.
Because of sea floor spreading
sea floor-spreading..;)
One key aspect that was not included in the support for Harry Hess's hypothesis of sea-floor spreading was the discovery of paleomagnetism, which provided evidence for the changing magnetic orientation of oceanic crust over time. While Hess focused on the process of new crust formation at mid-ocean ridges and its outward movement, the understanding of magnetic striping on the ocean floor, which was developed later, played a critical role in solidifying the theory. Additionally, Hess did not initially incorporate the concept of plate tectonics, which later integrated his ideas into a broader framework of geological processes.
by the plate tectonic and the ocean bridges
The researchers who used sonar to provide the first detailed evidence of sea floor spreading were Bruce Heezen and Marie Tharp in the early 1950s. Tharp's mapping of the Atlantic Ocean floor using sonar revealed the presence of the Mid-Atlantic Ridge and provided crucial support for the theory of plate tectonics.