neritic is near shore an covers about 1/4 of the ocean floor and pelagic is deep ocean basin and covers the other 3/4 of the ocean floor
Deposition is the process where sediments, like sand and soil, are deposited by wind, water, or ice. Over time, these sediments can build up in layers and form sedimentary rocks. Erosion and weathering play a crucial role in depositing sediments in different environments.
Many sediments end up in the ocean, where they are deposited on the seafloor. Others may accumulate in lakes, rivers, or on land. Over time, these sediments can become compressed and cemented together to form sedimentary rocks.
The rock is eroded or weathered away into sediments. The sediments settle and through compaction , the sediments are pushed together to form a sediment. Short Answer: It must be broken down into a sediment.
The process by which sediments are pressed together to form rock is called lithification. It involves the compaction of sediments due to the weight of overlying layers and the cementation of minerals to bind the sediment particles together. Over time, this process transforms loose sediments into solid rock.
Sediments can be picked up by water, wind, or ice. Water can transport sediments in rivers, streams, and oceans, while wind can carry sediments in the form of dust or sand. Ice, through processes like glaciers, can also transport sediments across landscapes.
They are formed in oceans as a result of pelagic sedimentation or precipitation
Deposition is the process where sediments, like sand and soil, are deposited by wind, water, or ice. Over time, these sediments can build up in layers and form sedimentary rocks. Erosion and weathering play a crucial role in depositing sediments in different environments.
Many sediments end up in the ocean, where they are deposited on the seafloor. Others may accumulate in lakes, rivers, or on land. Over time, these sediments can become compressed and cemented together to form sedimentary rocks.
Sediments form during the erosion and weathering processes that break down rocks into smaller particles. These sediments may then undergo deposition and compaction to form sedimentary rocks in the rock cycle.
Sedimentary rock.
Sediments have been transported over time through various natural processes such as erosion, weathering, and transportation by wind, water, glaciers, or gravity. These processes can move sediments from one location to another, shaping landscapes and depositing sediments in different environments. Eventually, these sediments can be compacted and cemented together to form sedimentary rocks.
The rock is eroded or weathered away into sediments. The sediments settle and through compaction , the sediments are pushed together to form a sediment. Short Answer: It must be broken down into a sediment.
Yes, basically sand is a form of sediment.
Hydrogenous sediments form when minerals precipitate directly from seawater as a result of chemical reactions or biological processes. For example, manganese nodules and phosphorite deposits are examples of hydrogenous sediments that form in this way in the deep sea. These sediments accumulate slowly over time on the ocean floor.
The action of water and gravity cause them to form in layers.
From Wikipedia: The neritic zone, also called the sublittoral zone[1], is the part of the ocean extending from the low tide mark to the edge of the continental shelf, with a relatively shallow depth extending to about 200 meters. The neritic zone has generally well-oxygenated water, low water pressure, and relatively stable temperature and salinity levels. These, combined with presence of light and the resulting photosynthetic life, such as phytoplankton and floating sargassum[2], make the neritic zone the location of the majority of sea life. Zooplankton, free-floating creatures ranging from microscopic diatoms to small fish and shrimp, live in this zone, and together with phytoplankton form the base of the food pyramid that supports most of the world's great fishing areas. At the edge of the neritic zone the continental shelves end, rapidly descending to the deeper oceanic crust and the pelagic zone.
because sediments has sand in it