Undisturbed seafloor sediments will carry a history of what has transpired there, much like glacial ice or peat bogs. Some interesting and potentially valuable mineral deposits are also found on the seafloor, eg. manganese nodules, metals from black smokers, and of course, deep in the rock, oil.
Most oceanic gas hydrates form when bacteria breaks down organic matter in seafloor sediments. The two types of biogenous sediments are calcareous ooze and siliceous ooze.
stuff from underwater
Microscopic Organisms.
The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
limestone, chalk, siltstone
Two types of biogenous sediments are calcareous ooze and siliceous ooze.
The ocean floor is composed of three different types of soil, known as pelagic sediments or marine sediments. They include calcareous ooze, red clay and siliceous ooze.
All sediments are solids by their very nature. By definition, a sediment is the solid material that settles out of a liquid suspension.
The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
Chert.
500 to 1000 meters
True.
sediments
limestone, chalk, siltstone
age increases
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
Sediments in geology are solid fragments of inorganic or organic material that come from the weathering of rock or biological processes and are carried and deposited by wind, water, or ice. Sediments are types of rock that are formed by the deposition of material from the Earth's surface. There are different types of sediments rocks.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
Age of seafloor rock and sediment increases with distance from the oceanic ridges.
bacteria break down organic matter in seafloor sediments