Geologic Time Flashcards
means that the forces and processes that we observe today have been at work for a very long time. This means that the forces that keep on changing Earth have been working for very long periods of time since the beginning of Earth’s history.
uniformitarianism
a Scottish geologist, proposed the principle of uniformitarianism
James Hutton
james hutton quote
“the present is the key to the past”
relative dating is determined by
stratified rocks
fossils
absolute dating is measured by
radioactive dating
fossils
A method of showing the sequence of events; that is, which happened first, next, and so on. For example, the rocks beneath a volcano were formed much ahead of the volcano, which means that a volcano is younger than the rocks beneath it.
relative dating
science that deals with the characteristics of layered rocks and how these rocks are used to trace Earth’s history
stratigraphy
formed over time by wind, rain and glacial formations. These rocks may be formed by folding and tilting, faulting, and volcanic intrusions.
stratified rocks
studied the relative positions of sediments in sedimentary rocks.
nicolas steno
states that in an undeform sequence of sedimentary rocks, each bed is older than the one above it and younger than the one below it.
law of superposition
states that sediments are deposited in flat layers. Thus, if the rock still maintains its horizontal layers, it means that it is not yet disturbed and still has its original horizontality.
Principle of Original Horizontality
states that when a fault cuts through rock layers, or when magma intrudes other rocks and crystallizes, we can assume that the fault or intrusion is younger than the rocks affected.
Principle of Cross-Cutting Relationships
Inclusions are rocks contained within other rocks. Rocks containing inclusions are younger than the inclusions they contain.
inclusions principle
rock layers that formed without interruption.
conformable
a layer of rock that was deformed or eroded before another layer was deposited, resulting in rock layers that are mismatched.
uncomformity
younger sediments rest upon the eroded surface of tilted or folded older rocks.
angular uncomformity
contact between younger and older beds is marked by a visible, irregular or uneven erosional surface.
disconformity