Clastic
Sedimentary rocks are primarily formed from deposited sediments, which can include fragments of igneous, metamorphic, and older sedimentary rocks. These sediments are transported by water, wind, or ice and accumulate in layers over time. Common types of sedimentary rocks include sandstone, limestone, and shale, which are formed from sand, biological materials, and clay, respectively. Additionally, volcanic ash can also contribute to sedimentary deposits.
when an organism is trapped in sedimentary rock, it will die and the organism will slowly decay, but it won't decay altogether and you get a fossil. the older the fossil is the lower down it will be in a sedimentary layer. that's called superposition...
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.
relative dating
No, radioactive isotopes in clastic sedimentary rocks can provide ages that are younger, older, or similar to the actual age of the rock. The key is to select an appropriate radioactive isotope with a suitable half-life that aligns with the age range of the sedimentary rock being studied.
Sedimentary rocks composed of older rocks are called "conglomerate" or "breccia." These rocks form when fragments of older rocks are compacted and cemented together to create a new rock.
Sedimentary rock is formed from the cementing of small pieces of older rocks, shells, soil, or dead plants and animals. These fragments, called sediments, can be compacted and cemented together over time to create sedimentary rock. Examples of sedimentary rocks include sandstone, limestone, and shale.
Classic sedimentary rocks are made up a minerals, grains, and rock fragments from older rocks. Some examples of this kind of rock are sandstone, breccia, and shale.
Radiometric dating is not usually effective for sedimentary rocks because they are formed from fragments of other rocks and do not contain the necessary minerals for radioactive decay dating to occur. Sedimentary rocks are composed of material that has been transported and deposited, which can result in a mixture of ages making it difficult to determine the exact age using radiometric dating methods.
Radiometric dating relies on the presence of radioactive isotopes that decay over time into stable isotopes. Sedimentary rocks are composed of weathered fragments of other rocks and minerals, so they do not usually contain the necessary radioactive isotopes for radiometric dating. This makes it difficult to directly date sedimentary rocks using radiometric methods.
The type of sedimentary rock in which the older rocks, unless disrupted, are on the bottom is called a fossil-rich limestone. This rock contains fossil remains of prehistoric organisms.
Clastic: These rocks are composed predominantly of broken pieces of older weathered and eroded rocksNon-clastic/ Organic: A sedimentary rock composed of the remains of plants and animals.just figure it out!
Sedimentary rocks are primarily formed from deposited sediments, which can include fragments of igneous, metamorphic, and older sedimentary rocks. These sediments are transported by water, wind, or ice and accumulate in layers over time. Common types of sedimentary rocks include sandstone, limestone, and shale, which are formed from sand, biological materials, and clay, respectively. Additionally, volcanic ash can also contribute to sedimentary deposits.
when an organism is trapped in sedimentary rock, it will die and the organism will slowly decay, but it won't decay altogether and you get a fossil. the older the fossil is the lower down it will be in a sedimentary layer. that's called superposition...
This type of sedimentary rock is called a "nonconformity." It occurs when younger sedimentary layers are deposited on top of older, often deformed or eroded, igneous or metamorphic rocks. Nonconformities indicate a significant gap in the geological record due to erosion or tectonic activity.
sedimentary
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.