There are three processes that add material to the ocean floor:
Sedimentation, and Vulcanism.
Sedimentation is usually caused by skeletons of sea animals falling to the ocean floor. It can be argued that this is not new material but only recycled materials. But some of the remains are calcium or other deposits that are added from land based run off. Silt deposits also run into the ocean floor from the land,
Vulcanism results from shifts in the ocean mantle with new material coming from deeper in the earth and spouting through volcanoes or emerging as new ocean floor at the rising edges of the tectonic plates.
Seafloor spreading occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away. Jennifer Castro
sea-floor spreading
sea-floor spreading
Sea floor spreading
The youngest rocks on the ocean floor are located at mid-ocean ridges, where new oceanic crust is constantly being formed through volcanic activity. These rocks are typically less than 5 million years old.
Lakes form on the floor of a rift valley due to the geological process of extensional tectonics, where the Earth's crust is being pulled apart. This creates a depression that can fill with water from rainfall or rivers, forming a lake. Rift valleys are often characterized by a series of interconnected lakes due to the topography and geology of the region.
Down the middle! The mid Atlantic ridge is a divergent plate margin along which new crust is constantly being produced.
the magnetic pattern on the sea floor
Exothermic is the process of heat being released. Wheat flour, in order to be produced, needs to have the reaction of heat treatment. The wheat flour is exothermic due to the treatment of heat.
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.
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.
when no more solids will dissolve into the watre a what is [produced
There are many things that could produced the ocean floor. Dying organisms for example are one component in the ocean floor.
A FLOOR PRODUCED FROM A MIXTURE of calcareous or silicious aggregates bonded with coalter pitch
sea-floor spreading
sea-floor spreading
FAlSE