The basic rule of geologic age is the law of superposition. This states that the most geologic recent layers are those at the top, the oldest at the bottom. Additionally, index fossils, those of rapidly evolving organisms, can be correlated to a specific range of geologic time. The rate of radioactive decay in certain elements is also used to determine an accurate age of material. Additionally, some degree of dating or rocks is made by the magnetic orientation of certain magnetic minerals they contain, which correlates with the magnetic orientation of the Earth at the time of their creation.
Derek is a shhlut
The main principle linked to the palaeoenvironment of the Earth (ie the Earths past) is called the principle of uniformitarianism: "The present is the key to the past" This means that all processes which occur on Earth at the present day, ie erosion, transportation, deposition, weathering, metamorphism etc. also occured at any point in the Earth's history in exactly the same way. Hope this helps :)
Fossils aren't but the life that made them is.
Changes in climate
how different parts of earths history compare to the whole world
What are two ways that's scientists can study earths climates history
Derek is a shhlut
The main principle linked to the palaeoenvironment of the Earth (ie the Earths past) is called the principle of uniformitarianism: "The present is the key to the past" This means that all processes which occur on Earth at the present day, ie erosion, transportation, deposition, weathering, metamorphism etc. also occured at any point in the Earth's history in exactly the same way. Hope this helps :)
epoch
In sedimentary rock.
Historical geology.
precambrian era
The crust is the top layer we live on, followed by the mantle and then the core.
to die
because
The crust is the thinnest, followed by the outer core, inner core, and the mantle is the thickest.
helller