Calcareous ooze
minerals that crystalize directly from ocean waters
It's material found in bottom sediment or in the water column of a body of water that was precipitated out of stuff in the water, ie. hydrogenous material does not come from a terrestrial, cosmic or biological source.
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.
Marine sediments are typically classified into four main classes: terrigenous, biogenous, hydrogenous, and cosmogenous. Terrigenous sediments originate from land, consisting of eroded rocks and soil transported by rivers and wind. Biogenous sediments are derived from biological materials, primarily the remains of marine organisms like foraminifera and diatoms. Hydrogenous sediments form directly from the precipitation of minerals from seawater, while cosmogenous sediments come from extraterrestrial sources, such as meteorites.
All hydrogenous sediments are formed from the precipitation of minerals directly from seawater. They typically consist of chemical compounds that crystallize out as a result of changes in water chemistry, temperature, or biological activity. Common examples include manganese nodules, phosphorites, and carbonates. These sediments often accumulate in specific marine environments, reflecting the local geochemical conditions.
not a hydrogenous sediment?
hydrogenous
Hydrogenous sediments are formed when minerals precipitate from the ocean, or they can be formed when minerals in the water react with older sediments.
minerals that crystalize directly from ocean waters
No, manganese nodules are examples of hydrogenous sediment. They form through chemical precipitation in seawater, often around a nucleus like a shark tooth or a shell, rather than being produced by living organisms like biogenous sediment.
Manganese nodules are an example of hydrogenous sediment, which forms directly from ocean water through chemical precipitation. They are typically found on the deep ocean floor.
Manganese nodules are polymetallic concretions found on the ocean floor and are formed through a slow process of precipitation and accumulation of manganese and other metals. They are a type of sediment known as hydrogenous sediment, as they form directly from seawater and not from the breakdown of rocks or organic materials.
Calcium oxide.
Chemical sedimentary rocks, such as limestone and chert, can form when minerals crystallize from seawater. These rocks are typically composed of minerals that precipitate out of solution in bodies of water, including oceans.
It's material found in bottom sediment or in the water column of a body of water that was precipitated out of stuff in the water, ie. hydrogenous material does not come from a terrestrial, cosmic or biological source.
Lithogenous sediment is not biogenous; it originates from the erosion of rocks on land. Biogenous sediments come from the remains of living organisms, such as shells and coral. Hydrogenous sediments are chemical precipitates that form in seawater.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.