Clastic rocks are sedimentary rocks consisting of bits and pieces of other rocks created by physical/mechanical weathering.
Non-clastic are also sedimentary rocks; however are absent bits and pieces of other rocks and are formed through chemical processes (e.g. hydrolysis, evaporation, precipitation, oxidation) or form out of organic material (e.g. coal, chalk).
== == Clastic sedimentary rocks.
They are classified as clastic or non-clastic. Clastic sedimentary rocks are formed from rock particles of various sizes. Non-clastic rocks are formed from precipitation of minerals out of solution or by the lithification of organic matter.
The difference between types of clastic rocks lies in their clast size, composition, and depositional environment. Some clastic sedimentary rock may consist of boulder sized fragments, others of microscopic sized particles. Shales will consist of clay minerals--sandstones usually consist of quartz minerals. Shale is from shallow marine deposition--sandstone from near shore or windblown deposition.
Clastic Rocks, Organic Rocks, and Chemical Rock
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.
clastic rocks are rocks that are broken off other rocks or sediments of rocks and come from many rocks through erosion nonfoliated is the opposite
Non-clastic is defined as a sedimentary rock that has a crystalline material. Non-clastic rocks are chemical sedimentary rocks made from biological activities including excretion and respiration.
Clastic and nonclastic
Clastic: These rocks are composed predominantly of broken pieces of older weathered and eroded rocks Non-clastic/ Organic: A sedimentary rock composed of the remains of plants and animals.
They are rocks.
== == Clastic sedimentary rocks.
They are classified as clastic or non-clastic. Clastic sedimentary rocks are formed from rock particles of various sizes. Non-clastic rocks are formed from precipitation of minerals out of solution or by the lithification of organic matter.
Clastic rocks are grouped based on the size of the grains of sediment contained within them.
The difference between types of clastic rocks lies in their clast size, composition, and depositional environment. Some clastic sedimentary rock may consist of boulder sized fragments, others of microscopic sized particles. Shales will consist of clay minerals--sandstones usually consist of quartz minerals. Shale is from shallow marine deposition--sandstone from near shore or windblown deposition.
Clastic Rocks, Organic Rocks, and Chemical Rock
the most common minerals in clastic sedimentary rocks are likely
They are all Sedimentary