rocks provide changes in the earth by telling us that dinasours were alive before humans and we can tell this because the skeletons of dinasours are buried deeper than human skeletons.
Scientists use the magnetic properties of some minerals as evidence of past changes in Earth's magnetic field. These changes can provide insight into the Earth's geological history, including continental drift and past climates.
The evidence includes seismic waves, which travel at different speeds and paths through Earth's interior. By analyzing how these waves behave, scientists have determined that Earth has distinct layers such as the crust, mantle, outer core, and inner core. Other evidence comes from the study of meteorites, which provide insight into the composition of Earth's layers.
To summarize, there are three types of geological evidence of the age of the earth. These are:Gradual processes of rock formationThe fossil recordRadioactive dating
The puzzle provided evidence of three types of changes on Earth's surface: the movement of tectonic plates resulting in earthquakes and mountain formation, erosion caused by wind and water shaping landscapes, and the impact of human activities such as deforestation and urban development altering the natural environment.
Physical evidence such as fossil records, geological formations, radioactive dating of rocks, and the distribution of species support the scientific theories of Earth's evolution over time. These pieces of evidence provide a timeline of Earth's history, showing changes in life forms and the environment over millions of years. Additionally, studies of plate tectonics and the geological record further support the concept of Earth's evolutionary processes.
One piece of evidence is the study of ancient rocks that show reversals in magnetic orientation. Another evidence comes from observations of the movement of the magnetic poles over time. Additionally, observations of magnetic anomalies in the Earth's crust provide further evidence of changes in the magnetic field.
Scientists use the magnetic properties of some minerals as evidence of past changes in Earth's magnetic field. These changes can provide insight into the Earth's geological history, including continental drift and past climates.
Earth's magnetic field reverses over time; the changes show that seafloor has taken place over time.
The evidence includes seismic waves, which travel at different speeds and paths through Earth's interior. By analyzing how these waves behave, scientists have determined that Earth has distinct layers such as the crust, mantle, outer core, and inner core. Other evidence comes from the study of meteorites, which provide insight into the composition of Earth's layers.
Limestone deposits that began as coral reefs provide how plate motions have changed Earth's surface. These deposits also provide evidence of past environments.
vibrations
To summarize, there are three types of geological evidence of the age of the earth. These are:Gradual processes of rock formationThe fossil recordRadioactive dating
because of pictures
Skeleton of dinosaurs are buried much deeper than human skeletons, therefore this shows that Dinosaurs were alive hundreds of years ago.
Biological evidence of the age of the earth includes the presence of fossils, the evolution of species over time as seen in the fossil record, and the molecular evidence of genetic changes in organisms that have accumulated over millions of years. These biological factors, along with others like radiometric dating of rocks, provide compelling evidence for the earth being billions of years old.
Wave Length.
yo but holeLimestone deposits that began as coral reefs provide evidence of how plate motions have changed Earth's surface. These deposits also provide evidence of past environments.