A lot of shells of marine organisms wind up on the ocean floor. Bones do not last on the ocean floor, they get eaten. But shells can last.
trench- valleys that form on the ocean floor where two plates come together, the deepest place in the ocean
yes
The rocks on either side of a mid-ocean ridge record the direction of the Earth's magnetic field at the time they were formed, and form a pattern of 'magnetic stripes' on either side of the ridge which are symmetrical. It is also now possible to measure ocean widths with sufficient accuracy to show yearly changes.
yes
Strips of ocean-floor basalt record the polarity of earth's magnetic field at the time the rock formed. These strips form a pattern that is the same on both sides of the mid-ocean ridge. the pattern shows that ocean floor forms along mid-ocean ridges and then moves away from the ridge.
trench- valleys that form on the ocean floor where two plates come together, the deepest place in the ocean
Sea Floor Spreading!
What causes ocean floor features to form
Organic things get buried in locations favourable for the formation of fossils (stream deltas, ocean floor.) The mud (or whatever) forms a hard cast about the thing. The thing then decomposes and gets flushed away. The hole fills with a mineral the local water is rich in. This is a fossil.
New material forms on the ocean floor of the mid-ocean ridge due to plate tectonics and volcanic activity. Volcanic eruptions deposit cooled magma on the ocean floor.
yes
New material forms on the ocean floor of the mid-ocean ridge due to plate tectonics and volcanic activity. Volcanic eruptions deposit cooled magma on the ocean floor.
they are called organic spots on the ocean floor.
Many fossils form because an animal dies and its body sinks to the ocean floor where it is buried in sediment. The bone sinks in the sediment and more is added on top. As the pressure increases the sediment turns into rock. The bone then dissolves from water and leaves a hole in its place. This natural mold is filled with minerals from the water. The area surrounding the fossil is then brought back to the surface after millions of years of erosion.
The rocks on either side of a mid-ocean ridge record the direction of the Earth's magnetic field at the time they were formed, and form a pattern of 'magnetic stripes' on either side of the ridge which are symmetrical. It is also now possible to measure ocean widths with sufficient accuracy to show yearly changes.
deep ocean currents form by the differences in the density of ocean water
Because i think there is more ocean than the land ; and ocean animals died more .,,