Location. Different layers of rock/soil tell a roughly chronological tale of the past, barring cataclysm. There are enough undisturbed sites worldwide that a mosaic can be discerned. Good question.
Mainly abrupt changes in mineral layers or the fossils in them.
In the order of time.
in the scope of geologic time, how significant is the presence of humans?
Measured rates of erosion.
eras and periods
Scientists first developed the geologic time scale by studying rock layers and index fossils worldwide. With this info. (information if you forget!), scientists placed Earth's rocks in order by the relative age.
The methods the geologists used when they first developed the geologic time scale. Were studying rock layers and index fossils worldwide. By Patrick
Scientists studied the layers of rock formations, fossils, and radioactive dating techniques to develop the geologic time scale. By analyzing the relative ages of rocks and fossils, as well as the decay of radioactive elements within them, scientists were able to divide Earth's history into distinct time periods.
I'm thinking it's index fossils because index fossils tell when or how old the layer it was found in. If that's what your asking.
Fossils found in the rock layer are the most accurate method for pinpointing a time period on the geologic time scale. By identifying the specific types of fossils present, scientists can determine the age of the rock layer relative to the known age ranges of those fossils.
becase scientists use it to place history in order
Humans
biologists
The information the geologic scale provides is animals and fossils over time and periods. Major divisions of time is called eras.
Mainly abrupt changes in mineral layers or the fossils in them.
biologists
Paleontologists, stratigraphers, and geochronologists worked with geologists to develop the geologic time scale. Paleontologists studied fossil evidence, stratigraphers looked at the layers of rock formations, and geochronologists used radiometric dating techniques to determine the age of rocks and fossils.