The sea floor bends down as a continental plate moves in the direction of the sea floor.
Less dense continental materials float over the more basaltic sea floor and sediments - this buoyant force lets the plate rise above the seafloor and push the sea floor down into the crust, following the descending edge of a convection cell in the crust, The area where this happens is called a subduction zone.
For a huge example, look at the west coast of North and South America where the Pacific is dragged beneath the continents. The hot rock , like a hot air balloon, rises through the continental crust, pushing it up and making mountains at the edge of the crustal plate. The rock stays so hot that it sometimes is pushed out the top of a mountain where the gases in the liquid rock expand like a soda shooting from a sealed bottle that has been shaken hard and opened suddenly, causing a volcanic eruption.
This process is not happening on the eastern coast of these two continents where the seashore goes at a gentle slope into the sea.
DA ANSWER ISseafloor spreadingThe_process_by_which_molten_material_adds_new_oceanic_crust_to_the_ocean_floor_is_calledThe_process_by_which_molten_material_adds_new_oceanic_crust_to_the_ocean_floor_is_called
To investigate the evolution of ocean basins by core drilling of ocean sediments and underlying oceanic crust.
the ocean sea floor is spreading
i think you mean what is the melting point of ice as water cant melt. the melting point of ice at sea level is 100 degres celsius
global warming has caused the polar ice caps to melt, this has caused sea level to rise
Basalt!
Probably consolidated sediments (sedimentary rock), then the rock basalt.
abyssal hills
Abyssal hills
Abyssal hills
true
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
As plankton die, it sinks to the sea floor, and over many years, a sediment is formed.
Sea floor bassalt and sediments.
Lithogenous sediments come from the land They result primarily from erosion by water, wind, and ice Biogenous sediments originate from organisms The particles in these sediments come from shells and hard skeletons. Although lithogenous sediments represent the largest total volume, biogenous sediments cover a greater area of sea floor
Metamorphic rocks can melt into magma and then undergo cooling and crystallization to become an igneous rock. Or, they can undergo weathering and erosion into sediments and then lithify to become sedimentary rocks. +++ They can melt and become magma only if subducted - a process normally confined to the sea-floor plate.
age increases