Deep-sea muds are primarily composed of fine-grained terrestrial material and are transported to the ocean floor by rivers or wind. Deep-sea oozes, on the other hand, are composed mainly of the calcareous or siliceous remains of microscopic marine organisms, such as foraminifera and diatoms, that accumulate on the ocean floor over time.
Deep-sea muds are primarily composed of fine particles like clay, silt, and sand that settle slowly from the water column. Deep-sea oozes, on the other hand, are specifically composed of the remains of planktonic organisms, such as foraminifera (calcium carbonate) or diatoms (silica), which accumulate on the seafloor over time.
The two types of biogenous sediments are siliceous oozes, which are made up of silica-based remains of diatoms and radiolarians, and calcareous oozes, which consist of calcium carbonate shells of organisms like foraminifera and coccolithophores.
Calcareous oozes form when the calcium carbonate shells and skeletons of marine organisms, such as foraminifera and coccolithophores, accumulate on the ocean floor. Over time, these calcareous remains compact and cement together to form a sediment known as calcareous ooze.
What they are made of. Calcareous ooze is made from calium carbnate shells of cooclithophores, foraminifera, and other things with carbonate shells. Siliceous ooze is made of silica shells of radiolaria (really cool looking), diatoms, and anything else with a silica shell.
This is called a rift. Rifts form when the Earth's crust is being pulled apart by tectonic forces, creating a gap where magma can rise up from the mantle and solidify to form new crust. Rift valleys like the East African Rift are examples of this geological process in action.
oozes are from organic material; deep-sea muds from inorganic
oozes:organic deep-sea:inorganic
Deep-sea muds are primarily composed of fine particles like clay, silt, and sand that settle slowly from the water column. Deep-sea oozes, on the other hand, are specifically composed of the remains of planktonic organisms, such as foraminifera (calcium carbonate) or diatoms (silica), which accumulate on the seafloor over time.
every volcano either oozes lava, ash, or rock
Yes, magma oozes from the cracks at mid-ocean ridges.
Yes, magma oozes from the cracks at mid-ocean ridges.
Yes, magma from the earth oozes from the cracks at mid-ocean ridges.
Yes, magma oozes from the cracks at mid-ocean ridges.
Yes, magma oozes from the cracks at mid-ocean ridges.
lava
It's called pus.
Limestone is a sedimentary rock that is made from lime oozes. It forms from the accumulation and lithification of calcium carbonate-rich sediments deposited in marine environments.