biological precipitation
Chalk formed from sediments made of skeletions of microscopic living things in the ocean must be a(n) organic rock.
The sediments that do consists of mostly microscopic shells and hard parts of organisms is Clay.
radiolaria; foraminifera radiolaria(single-celled animals) forminifera(marine plankton species)
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.
Lithogenous sediments come from the land They result primarily from erosion by water, wind, and ice Biogenous sediments originate from organisms The particles in these sediments come from shells and hard skeletons. Although lithogenous sediments represent the largest total volume, biogenous sediments cover a greater area of sea floor
Biogeneous sediments
it is the state of being depositing or precipitated
Terence P. Scoffin has written: 'An introduction to carbonate sediments and rocks' -- subject(s): Carbonate Rocks, Carbonates, Sediments (Geology)
Deposition is the state of being deposited or precipitated as in the deposition of soil at the mouth of a river.
Chalk formed from sediments made of skeletions of microscopic living things in the ocean must be a(n) organic rock.
The sediments that do consists of mostly microscopic shells and hard parts of organisms is Clay.
The sediments that do consists of mostly microscopic shells and hard parts of organisms is Clay.
The sediments in sedimentary rock are held together by precipitated cementing material which is commonly silicate, carbonate, clay, or iron in composition.
radiolaria; foraminifera radiolaria(single-celled animals) forminifera(marine plankton species)
the places in which fossils can be formed in incorporated sediments and rocks in the bottom of the sea.this shows the formation of petroleum from rock sediments under the sea,because this decay is a scheme which take millions of years.maven
It gets transported from one place to another
Clastic sedimentary rocks. Clastic sedimentary rocks are formed when small sediment particles are compacted and cemented together. This happens when the sediments are glued together by tiny crystals or chemicals from fluids that have precipitated in the pores between the sediments.