Deep ocean trenches were found near some of the continental landmasses, particularly around the edges of the Pacific. It turned out that some of the deepest parts of the ocean are actually near some of the continents, and out in the middle of the oceans the water is relatively shallow because of the underwater mountains. Volcanic activity and lots of heat were discovered near the underwater mountains. With this new information, H. H. Hess, an American geologist, presented the hypothesis of seafloor spreading.
The evidence for seafloor spreading includes the discovery of mid-ocean ridges, magnetic striping patterns on the ocean floor, and the age of oceanic crust becoming younger as it moves away from these ridges. Additionally, studies of earthquake activity and ocean drilling have provided further support for the theory.
Pillow lava forms when molten lava erupts underwater and cools rapidly, creating characteristic pillow-like structures. This type of lava is commonly found along mid-ocean ridges, which are areas where sea-floor spreading occurs. The presence of pillow lava on the ocean floor is evidence of volcanic activity associated with sea-floor spreading.
provide evidence for sea-floor spreading
Spreading Of ocean floor
Mapping of magnetic anomalies on the ocean floor shows alternating bands of normal and reversed polarity, indicating that new oceanic crust is continuously forming at mid-ocean ridges and spreading away in opposite directions.
Yes, the analysis of sea-floor sediments can provide evidence of sea-floor spreading. By studying the age and composition of the sediments, scientists can track the movement of tectonic plates and the spreading of the sea floor over time. Additionally, magnetic anomalies recorded in these sediments can further support the theory of sea-floor spreading.
Magnetic minerals on the ocean floor.
by the plate tectonic and the ocean bridges
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.
sea floor-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.
seafloor spreading, age of the sea floor and ocean trenches.
Pillow lava forms when molten lava erupts underwater and cools rapidly, creating characteristic pillow-like structures. This type of lava is commonly found along mid-ocean ridges, which are areas where sea-floor spreading occurs. The presence of pillow lava on the ocean floor is evidence of volcanic activity associated with sea-floor spreading.
because
provide evidence for sea-floor spreading
Spreading Of ocean floor
Evidence shows that molten material erupts through this valley. The material then hardens to form the rock of the ocean floor.-Answered by Nadezda Dimsoski
Ocean-floor rocks near mid-ocean ridges show a symmetrical pattern of magnetized stripes parallel to the ridge axis. These stripes result from periodic reversals in Earth's magnetic field and provide evidence of seafloor spreading. Sediments on the ocean floor also show younger ages near the ridges, supporting the idea of seafloor spreading.