The oldest layers of sea floor would exist at the bottom of the Marianas Trench, where oceanic plate subduction is occurring. The subducting oceanic plate is less than 200 million years in age.
The oldest rocks on the continents would be much older than the rocks on the sea floor because the rocks on the continents are not being removed unlike the rocks on the sea floor that are made by the mid-ocean ridge are being removed by deep ocean trenches. this prossess that is occuring on the sea floor is called sea floor spreading. evidence of this is the Pacific ocean shrinking and the Atlantic ocean growing.
The banding pattern of rocks on either side of mid-ocean ridges shows symmetrical stripes of magnetic reversals, indicating that new crust is formed at the ridge and then moves outward as tectonic plates diverge. This magnetic pattern correlates with the age of the rocks, with younger rocks found closer to the ridge and older rocks further away. The consistent dating of these rocks supports the theory of sea floor spreading, demonstrating that new oceanic crust is continuously generated while older crust is pushed away. Together, these patterns provide strong evidence for the dynamic processes of plate tectonics and sea floor spreading.
sea-floor spreading
Forms by lava from volcanoes on the sea floor
provide evidence for sea-floor spreading
Yes
Sea Floor Spreading
Sea Floor Spreading
Sea floor rocks are young because of the process of seafloor spreading at mid-ocean ridges. As new oceanic crust forms at the ridges, older rocks get pushed further away. This continuous process creates a relatively young age for the sea floor rocks, with the oldest rocks being around 200 million years old.
same age. the ice caps just melted on top over the rocks at the bottom of the sea.
The oldest rocks on the continents would be much older than the rocks on the sea floor because the rocks on the continents are not being removed unlike the rocks on the sea floor that are made by the mid-ocean ridge are being removed by deep ocean trenches. this prossess that is occuring on the sea floor is called sea floor spreading. evidence of this is the Pacific ocean shrinking and the Atlantic ocean growing.
The evidence that rocks farther from a ridge are older than rocks closer to the ridge supports the idea of sea floor spreading because it aligns with the concept of a divergent boundary where new oceanic crust is continuously formed at the ridge and gradually moves away from the ridge over time. This process allows for the creation of age gradients in the oceanic crust, with the youngest rocks found near the ridge and progressively older rocks located farther away.
Around 200 million years of age.
The banding pattern of rocks on either side of mid-ocean ridges shows symmetrical stripes of magnetic reversals, indicating that new crust is formed at the ridge and then moves outward as tectonic plates diverge. This magnetic pattern correlates with the age of the rocks, with younger rocks found closer to the ridge and older rocks further away. The consistent dating of these rocks supports the theory of sea floor spreading, demonstrating that new oceanic crust is continuously generated while older crust is pushed away. Together, these patterns provide strong evidence for the dynamic processes of plate tectonics and sea floor spreading.
Harry Hess hypothesized that the sea floor was spreading. He explained it through the phenomena of the youngest rocks that are found only at the mid-ocean ridges. These rocks then, get progressively older when moving away from the ridge.
sea-floor spreading
Forms by lava from volcanoes on the sea floor