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Two primary types of sediments on ocean bottom?

There are two types of deep ocean sediments, abyssal clay and biogenous oozes. Abyssal clays are fine-grained sediment, while biogenous ooze is composed of the hard parts of microscopic organisms.


How does a fluke style anchor hold a recreational boat in place?

By burring into the bottom sediments


What is layers of sediment forming at the bottom of the ocean called?

Layers of sediment forming at the bottom of the ocean are called "marine sediments." These sediments are made up of a variety of materials such as mineral particles, organic matter, and remains of marine organisms, which accumulate over time to form distinct layers.


Where is benthos located?

Benthos is a term for bottom-dwelling (i.e. on, in, or very near) organisms because they live on the seabed (what is known as the "benthic zone"). There are different classifications though: the epifauna live on the sea bottom and infauna live in the sediments on the sea bottom.


Does plankton eat aquatic plants?

No, plankton are microscopic plants and animals. They either make their own food from sunlight or eat other microscopic organisms.


When sediments are disturbed the oldest layers are found at the?

In disturbed sediments without layers, the relative age of the sediments would be unknown.


How is limestone formed in Florida?

over a very long time layers of these sediments hardened into a sedimentary rock called limestone


What happened to sediments in the presence of gravity?

They sink to the bottom.


What is a loose material that sinks to the bottom of water?

Sediments


What is Minerals and debris that settle at the bottom of a river are called?

sediments


What does river deposit mean?

accumulated sediments on the bottom of the river


Where are the oldest layers of sediments located?

The oldest layers of sediments are typically found at the bottom of a sedimentary rock sequence, with the youngest layers at the top. Over time, new layers of sediments accumulate on top of older layers, creating a chronological sequence with the oldest layers at the bottom.