Geology 101 Quiz 9 Flashcards
two types of age determination
relative and absolute dating
relative dating
finding the age relative to another object or event (younger or older)
absolute dating
finding the age in years
absolute dating has only been possible since the discovery of ? at the start of the ? century
radioactivity; 20th
principle of original horizontality
sedimentary layers, called strata, were deposited nearly horizontally
principle of superposition
younger sediments are deposited on top of older sediments
in undisturbed strata, the ? layer will always be the youngest
upper
the order of the layers repeats itself
thrust fault
when a fold has been pushed over onto itself - strata repeat, but in the middle of the repeating layers, an additional repeated set is upside down
overturned fold
principle of original lateral continuity
identical layers on opposite sides of a valley were once continuous
principle of inclusions
if a rock contains fragments of rock from an adjacent unit, the adjacent unit must be older
principle of cross-cutting relationships
younger rock or features cut across older rocks or features
uncomformity
an eroded surface
index fossil
a fossil organism with widespread distribution that existed for a short time span
use of index fossils
only organisms that are widespread and with a relatively short time of existence are useful for relative dating
index fossils appear out of order because of
alteration of the strata after deposition
geologic column
early geologists had no knowledge of the absolute age of various layers in the sequence, so they assigned names to each time interval (Jurassic, Cretaceous, Cambrian)
absolute dating synonyms
isotopic dating, radiometric (measurements using radioactivity) dating
radioactive isotopes are atoms that have
either too many or too few neutrons in the nucleus that results in an unstable arrangement (some arrangements are more unstable than others, resulting in faster rates of decay)
decay refers to
a spontaneous change in the number of protons and neutrons in the nucleus of the atom by either ejecting some of them, or by converting a proton into a neutron or a neutron into a proton (a new element is created b/c # protons changes)
half life
the time required for half the radioactive atoms to decay
is decay linear?
no, this is why we use half lives - decay is exponential
the more unstable the nucleus, the (less/more) radioactive the isotope and the (shorter/longer) the half life
more; shorter
limits on radioactive dating
- rock must contain a detectable concentration of the isotope being used
- the age of the rock must be within about 6 to 12 half lives of the isotope being used (depending on the method)
- enough time must pass for daughter products to appear in measurable quantity
- pay attention to what is being dated
ways to date sedimentary rocks
- proximity to datable igneous rocks
2. use of index fossils
proximity to datable igneous rocks to date sedimentary rocks
if datable igneous rocks are associated with the sedimentary rock, it may be possible to bracket the possible age of the sedimentary rock, or at least assign an upper or lower age limit
proximity example: if sandstone is between a two layers of ash 11 to 15 million years old, its age is likely
within 11-15 million years old
proximity example: if sandstone is between two sills 11 to 15 million years old, its age is likely
greater than 15 million years because sills intrude
use of index fossils to date sedimentary rocks
if one of the index fossils is found in sedimentary rocks, the absolute age (or at least a range) can be assigned to the rocks even if there are no ash deposits or other directly datable rocks
how do we know isotope dating methods are accurate?
- radioactive decay rates have been shown to be constant under a wide range of temperatures, pressures, and chemical reactions
- multiple isotope methods, based on different sets of assumptions, typically give comparable results
- in some cases, non radioactive methods can be used to estimate an age that can then be compared with isotope methods