Historical Geology Flashcards
– placing rocks in their proper sequence of formation, first, second, third, and so on.
Relative Dating
– it states that in an underformed sequence of sedimentary rocks, each bed is older that the one above it and younger than the one below.
Law of Superposition
- it means that layers of sediment are generally deposited in a horizontal position
Law of Original Horizontality
When a fault cuts through other rocks, or when magma
intrudes and crystallizes, we can assume that the fault or intrusion is younger than the rocks affected
Principle of Cross Cutting
these are pieces of one rock unit that are contained within another. The rock mass adjacent to the one containing the inclusions must have been there first in order to provide the rock fragments. Therefore, the rock mass containing inclusions is the younger of
the two
Inclusions
represents a long period during which deposition ceased, erosion removed previously formed rocks, and then deposition resumed.
Unconformity
It consists of tilted or folded sedimentary rocks that are
overlain by younger, more flat-lying strata
Angular Unconformity
are more common but usually far less conspicuous because the strata on either side are essentially parallel
Disconformity
the break separates older metamorphic or intrusive igneous rocks from younger sedimentary strata
Nonconformity
the remains or traces of prehistoric life. An important inclusions in sediment and sedimentary rocks
Fossils
an interdisciplinary science that blends geology and biology in an attempt to understand all aspects of the succession of life over the vast expanse of
geologic time
Paleontology
the small internal cavities and pores of the original structure are filled with precipitated mineral matter
Petrified
the cell walls and other solid material are removed and replaced with mineral matter.
Replacement
Created when a shell or other structure is buried in sediment and then dissolved by underground water,
Mold
It occurs when fine sediment encases the remains of an organism
Carbonation
- If the film of carbon is lost from a fossil preserved in fine-grained sediment, a replica of the surface that may show considerable detaail
Impression
created when hollow spaces are subsequently filled with mineral matter
Cast
these are the traces of prehistoric life
Trace Fossil
animal footprints made in soft sediment that was later lithified
Tracks
fossil dung and stomach contents that can provide useful informationpertaining to food habits of organisms
Coprolite
highly polished stomach stones that were used in the grinding of food by some extinct reptiles
Gastroliths
an English engineer and canal builder who discovered that each rock formation in the canals he worked on contained fossils unlike those in the beds either
above or below
William Smith
These fossils are widespread geographically and are limited to a short span of geologic time, so their presence provides an important method of matching rocks of the same age
Index Fossil
contains the protons and neutrons of an atom and is orbited by electrons.
Nucleus
number of protons in the nucleus.
Atomic Number
derived by adding the protons and neutrons in an atom’s nucleus
Mass Number
Varieties of the same element that have different mass numbers; their nuclei contain the same number of protons but different numbers of neutrons
Isotopes
The spontaneous decay of certain unstable atomic nuclei
Radioactivity
an unstable isotope of an element
Parent
the isotopes resulting from the decay of the parent
Daughter Product
The procedure of calculating the absolute ages of
rocks and minerals containing certain radioactive isotopes
Radiometric Dating
The time required for half of the nuclei in a sample to decay
Half Life
dating recent events with the use of carbon-14
radioactive isotopes
Radiocarbon Dating
The dating and study of annual rings in trees
Dendrochronology
represent the greatest expanses of time
Eons
a major division on the geologic time scale
Era
characterized by a somewhat less profound change in life-forms as compared with the eras
Period