When the sea floor is thickest, it typically forms a broad, elevated feature known as a mid-ocean ridge. This occurs due to tectonic activity, where magma rises to the surface, creating new oceanic crust. Additionally, sediment accumulation can contribute to the thickness in certain areas, resulting in a varied topography that includes features like seamounts and abyssal plains. Overall, the sea floor's thickness can create a series of ridges and valleys, reflecting the dynamic processes of plate tectonics.
sea-floor spreading
Sea floor spreading occurs when new oceanic crust is formed at mid-ocean ridges and pushes the existing crust apart. As the new crust cools and solidifies, it creates a symmetrical pattern where the ocean floor becomes wider. This process alters the shape of the ocean floor by creating a series of parallel ridges and valleys.
It is the thickest under mountains ranges.
Forms by lava from volcanoes on the sea floor
The Super Continent was broken apart, in part by sea-floor spreading.Scientists discovered that sea-floor spreading continues to move the continents.Sea-floor spreading can be measured using specialized equipment.
subduction and sea floor spreading.
they use a camera X)
by far polar bear because the live in much colder weather then sea otter
the theory of sea floor spreading or continental drift
they have the thickest coat of all mammals
sea-floor spreading
They are volcanic in origin, conical in shape and at least 1000 metres above the ocean floor
a Polyp.
It was created on the sea floor.
Sea floor spreading occurs when new oceanic crust is formed at mid-ocean ridges and pushes the existing crust apart. As the new crust cools and solidifies, it creates a symmetrical pattern where the ocean floor becomes wider. This process alters the shape of the ocean floor by creating a series of parallel ridges and valleys.
the sea floor separates. magma comes up the crack forming new sea floor
It is the thickest under mountains ranges.