seafloor spreading by Harry Hess
The region where the seafloor is forced beneath the continental plate is called a subduction zone. When the seafloor descends down it produces a deep-ocean trench.
At divergent plate boundaries the spreading of the tectonic plates results in the reduced pressure of the underlying magma. As the spreading continues, lava fills in the area of spreading and cools, becoming the newest addition to the seafloor. This process occurs at a steady rate ranging from a few centimeters to several centimeters of new sea floor each year. However, at a different location opposite the newly formed seafloor are convergent plate boundaries where land and seafloor is destroyed to make room for new seafloor.
The Benthic Zone
biochemist
The thicker the slab of seafloor, the more material it contains, leading to a greater weight. This weight is influenced by the density of the rock forming the seafloor. Thicker slabs of seafloor would have more mass and therefore weigh more than thinner slabs.
The process is called subduction. This occurs at convergent plate boundaries, where one of the plates is forced beneath the other due to differences in density. The melting of the subducted plate creates magma that can eventually lead to volcanic activity.
The amount of seafloor sediments can vary widely depending on location. Generally, it ranges from a few centimeters to several kilometers thick. Factors such as proximity to land, ocean currents, and sediment sources influence the accumulation of sediments on the seafloor.
Hess proposes seafloor spreading
ocean
Seafloor Spreading
Seafloor Spreading
Rocks in the seafloor are moving one place to another
seafloor spreading
large regions of the seafloor that appear flat but are not
Henry H. hess
whatis the flat part of the seafloor called?