Organic sedimentary rock is primarily composed of the remains of living organisms, particularly plants and animals. Common types include coal, formed from compressed plant material, and limestone, which can contain the shells and skeletal fragments of marine organisms. These rocks typically accumulate in environments like swamps and ocean floors, where organic material can be preserved over time. The lithification process then turns this organic material into solid rock through compaction and cementation.
Clastic sedimentary rock forms when fragments of preexisting rocks are compacted or cemented together. Organic sedimentary rock forms from the remains of plants or animals. Chemical sedimentary rock forms when minerals precipitate from a solution or settle from a suspension.
Sedimentary rock formed from pieces of once living organisms is called organic or biogenic sedimentary rock. This type of rock is made up of the remains of plants or animals that have been compacted and cemented together over time. Examples include limestone, coal, and chalk.
sedimentary, erosion products and/or organic matter that has become glued together over time into rockmetamorphic, sedimentary or igneous rock that has been changed in form by very high temperature and pressure while deep undergroundigneous, solidified by cooling from molten rock
is a mixture of organic chemical compounds that make up a portion of the organic matter in sedimentary rocks.
The size of the grains that make up the rock
An Organic rock is an Sedimentary rock and it is made in the ocean from calcium and other minerals building up on the ocean floor :)
This type of sedimentary rock is called organic sedimentary rock. It forms from the accumulation and compaction of plant and animal remains, such as shells, skeletons, and plant materials. Common examples include limestone, coal, and chalk.
Rock salt is a chemical sedimentary rock.
Sedimentary rocks are classified according to the types of particles that make up the layers of rock. These particles can include minerals, organic matter, and even fragments of other rocks that have been eroded and transported by water, wind, or ice before being deposited and lithified into layers of sedimentary rock.
Clastic sedimentary rock forms when fragments of preexisting rocks are compacted or cemented together. Organic sedimentary rock forms from the remains of plants or animals. Chemical sedimentary rock forms when minerals precipitate from a solution or settle from a suspension.
Sedimentary rock, specifically organic sedimentary rock such as coal or limestone, forms where the remains of plants and animals are deposited in thick layers over time. These rocks are primarily made up of organic material and are created through the compression and cementation of these remains.
There are several environmental changes that can stop the development of an organic sedimentary rock. These changes include: global warming, sudden cooling, lowering of the sea levels and drastic changes in pH levels.
Sedimentary rock formed from pieces of once living organisms is called organic or biogenic sedimentary rock. This type of rock is made up of the remains of plants or animals that have been compacted and cemented together over time. Examples include limestone, coal, and chalk.
An organic sedimentary rock composed of cemented shells is called limestone. Limestone is primarily made up of the mineral calcite, which is derived from the shells of marine organisms like coral and mollusks. Over time, these shells accumulate and compress to form solid rock.
Clasts are individual pieces of rock or mineral fragments that make up a sedimentary rock. They can vary in size and shape, ranging from tiny grains to large boulders, and are important in determining the characteristics and composition of the sedimentary rock.
sedimentary, erosion products and/or organic matter that has become glued together over time into rockmetamorphic, sedimentary or igneous rock that has been changed in form by very high temperature and pressure while deep undergroundigneous, solidified by cooling from molten rock
is a mixture of organic chemical compounds that make up a portion of the organic matter in sedimentary rocks.