Lithogenous sediment particles are produced by wind and water erosion and weathering of terrestrial rocks. During weathering, easily dissolved minerals are removed, leaving mostly siliceous minerals including quartz, feldspars, and clay minerals. Clay minerals are layered structures of silicon, aluminum, and oxygen atoms, some containing iron and other elements. They are then carried to the oceans by rivers, glaciers, and winds, or eroded from Coastlines by waves.
because biogenous ooze is the mmst common pelagic deposits
Sedimentary rocks are formed by the lithification (cementing, compacting, and hardening) of existing rock or the bones, shells, and pieces of formerly living things. Rocks are weathered and eroded into tiny particles which are then transported and deposited along with other pieces of rock called sediments. Sediments are cemented together and compacted and hardened over time by the weight and pressure of up to thousands of feet of additional sediments above them. Eventually, the sediments are lithified and become solid sedimentary rock. These sediments that come together are known as clastic sediments. Sediments usually sort themselves by the size of the particles during the deposition process so sedimentary rocks tend to contain similarly sized sedimentary particles. An alternative to clastic sediments are chemical sediments which are minerals in solution that harden. The most common chemical sedimentary rock is limestone, which is a biochemical product of calcium carbonate created by the parts of dead creatures. Approximately three-quarters of the earth's bedrock on the continents is sedimentary.
well, beaches are made of sediments and both are rocks broken down into smaller pieces
they have in common their both particles
There are a few other words that mean the same as 'conveyed'. Some of the most common words are sent, transmitted, siphoned, granted, transferred and carried.
Bioturbation refers to the reworking and mixing of sediments due to biologic activity. Worms and other burrowing organisms are common producers of bioturbated sediments.
Common sedimentary rocks include sandstone, limestone, and shale. These rocks often start as sediments carried in rivers and deposited in lakes and oceans. When buried, the sediments lose water and become cemented to form rock.
Moraines, erratic blocks and clay with flints are some.
Deposition of continental sediments
Erosion and sediments from large rivers.
they both have particles in them.
it have small particles