Biochemical rock is characterized by the presence of organic materials or fossils that indicate biological activity in its formation. This type of rock often contains remains of plants and animals, such as shells or coral, and is typically formed through the accumulation of biological debris. Common examples include limestone, which can form from coral reefs or shell deposits, and coal, which originates from plant material. The organic origin distinguishes biochemical rocks from other sedimentary types.
The rough estimating of the age of a fossil or rock containing fossils is called relative dating, and is based on the position of the rock or fossil in undisturbed sedimentary strata which contains what are called 'index fossils', fossils that only appear in specific geologic time periods.
fossils are fine in metamorphic rock
Fossils are formed in sedimentary rock because the rock is formed at temperatures that do not destroy the fossils like the igneous rocks would.
Fossils can be used to determine the relative age of rock layers by comparing the types of fossils found in different layers. Fossils of organisms that existed for a short period of time can be used to date layers of rock containing them. Geologic features such as fault lines and unconformities can also help determine the relative age of rock layers by showing where layers have been disturbed or eroded.
Limestone is a biochemical rock that can contain fossils. It is formed from the accumulation of calcite or aragonite shells or skeletal fragments of organisms such as corals, foraminifera, and mollusks. Over time, these remains can be compressed and preserved in the rock.
Paleontologists are looking for fossils in sedimentary rock.
The Adirondack rocks have been both severely folded and sheared by ductile deformation and shattered by brittle.
fossils
sedimentary
They Often Contain fossils.
Index fossils are fossils of organisms that lived for a relatively short period of time but were widespread geographically. By identifying these index fossils in a particular layer of rock, scientists can determine the age of the rock and correlate it with other rock layers containing the same index fossils. This allows for the relative dating of rock layers based on the presence of specific index fossils.
Biochemical rock is characterized by the presence of organic materials or fossils that indicate biological activity in its formation. This type of rock often contains remains of plants and animals, such as shells or coral, and is typically formed through the accumulation of biological debris. Common examples include limestone, which can form from coral reefs or shell deposits, and coal, which originates from plant material. The organic origin distinguishes biochemical rocks from other sedimentary types.
No rock could be a biochemical.
fossils
Quite often, fossils are contained within shale rock.
The rough estimating of the age of a fossil or rock containing fossils is called relative dating, and is based on the position of the rock or fossil in undisturbed sedimentary strata which contains what are called 'index fossils', fossils that only appear in specific geologic time periods.