
deep sea sediment
Deep sea sediment refers to the layers of particles, minerals, and organic material that settle on the ocean floor in the deep, dark parts of the world's oceans. These sediments are formed from a combination of tiny pieces of rocks, shells, dead micro-organisms, and organic matter that drift down from the surface. Over time, they accumulate to create thick layers, providing valuable information about Earth's history, climate change, and ocean processes. Studying deep sea sediments helps scientists understand past environments and predict future changes affecting our planet.