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What process is not involved in making of clastic rocks?

build-up of plants materials


what process is NOT involved in the making of clastic rocks?

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Of the following the only process NOT involved in the making of clastic rocks is what?

Crystallization is not involved in the making of clastic rocks. Clastic rocks are formed through the accumulation and cementation of loose rock fragments, called clasts, through processes like weathering, erosion, transportation, and deposition. Crystallization typically refers to the formation of crystals from a liquid or gas, and is more commonly associated with the formation of igneous or metamorphic rocks.


How do clastic rocks differ from non clastic rocks in terms of process of formation?

Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.


How do clastic rocks differ from non-clastic rocks in terms of process of formation?

Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.


What major process in the formation of clastic sedimentary rocks is .?

Cementation


Is sediment transport invovled in the making of clastic rocks?

Yes, sediment transport is a crucial process in the formation of clastic rocks. Clastic rocks are formed from the accumulation and lithification of sediments, which are typically derived from the weathering and erosion of pre-existing rocks. These sediments are transported by natural agents such as water, wind, or ice before being deposited in various environments, where they compact and cement over time to form clastic rock types, such as sandstone and shale.


How does clastic rocks differ from non -clastic in terms of process of formation?

Clastic rocks are formed from the accumulation and cementation of fragments of pre-existing rocks and minerals, typically through processes like weathering, erosion, and deposition. In contrast, non-clastic rocks, such as chemical or organic sedimentary rocks, form through different processes, including the precipitation of minerals from solution or the accumulation of organic matter. While clastic rocks are primarily composed of solid particles, non-clastic rocks often involve chemical reactions or biological activity in their formation. This fundamental difference in formation processes leads to distinct physical and chemical characteristics between the two types of rocks.


How are clastic rocks grouped?

Clastic rocks are grouped based on the size of the grains of sediment contained within them.


What do clastic and chemical rocks have in common?

Clastic and chemical rocks are both types of sedimentary rocks. They form from the accumulation and cementation of sediment particles. Clastic rocks are composed of fragments of pre-existing rocks, while chemical rocks form from the precipitation of minerals from water solutions.


What are the three categories of sedimentary rocks?

The three categories of sedimentary rocks are clastic, chemical, and organic. Clastic rocks form from the accumulation of weathered rock fragments, chemical rocks form from the precipitation of minerals from water, and organic rocks form from the remains of living organisms.


Difference between clastic rocks and non-clastic rocks?

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).