The current geologic age is referred to as the Holocene epoch.
No movement
I think you are going for plate tectonics.
The diagram accurately represents geologic time by showing the relative ages of rock layers or fossils through superposition. It also conveys the concept of uniformitarianism, illustrating the gradual changes that have occurred over millions of years. Additionally, the diagram may incorporate index fossils to help correlate rock layers from different locations and determine relative ages.
The early geologic time scale did not include specific numerical ages for events because it was primarily based on the relative dating of rock layers and the fossils they contained, rather than absolute dating methods. Scientists relied on the principles of stratigraphy and biostratigraphy to establish the sequence of geological events without assigning precise dates. It wasn't until the development of radiometric dating techniques in the early 20th century that geologists could accurately quantify the ages of rocks and events, leading to the modern geologic time scale that includes specific timeframes.
Unconformity
James Hutton discovered the uniformitarianism theory, which states that the earth has changed and is still changing overtime, but very slowly.
The current geologic age is referred to as the Holocene epoch.
A palaeopolyploidization is the development of polyploid organisms in the geologic past.
Seafloor spreading
Geologic features are physical attributes of the Earth's surface that are a result of geological processes over time. These features include mountains, valleys, oceans, volcanoes, and plateaus, among others. They provide valuable insights into the Earth's history and the processes that have shaped its landscape.
Seafloor spreading
No movement
I think you are going for plate tectonics.
To have a scientist make a geologic map, they need to know something about geologic formation to show what the map is meaning. They use color to show the differences of the kind of rock and its age.
eon>era>period
Heat presshure melting weathering erosion compacting cementing and cooling