Lab 9 Flashcards

(36 cards)

1
Q

What are the 5 principles of Stratigraphy

A

Principle of Superposition
Principle of Original Horizontality
Principle of Cross-Cutting relations
Principle of Inclusions
Principle of Fossil Succession

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2
Q

Describe the Principle of Superposition

A

In an undisturbed sequence of rocks, the oldest rocks are at the bottom and the youngest at the top. If it is found to be the reverse, the sequence must have been overturned at some point

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3
Q

Describe the principle of Cross-Cutting Relations

A

If a rock unit is cross-cut by another feature such as a fault or igneous intrusion, the feature that cuts across is younger than the rock unit which is dissected

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4
Q

Describe the Principle of Original Horizontality

A

All waterline sediments were deposited horizontally (or nearly so). If sedimentary rocks are found tilted or overturned, this was due to a later event. This principle only determines the relative time of the tilting event (often the tilting is due to the beds being part of large scale folds)

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5
Q

Describe the principle of Inclusions

A

When a rock unit contains fragments of another rock within it, those fragments represent a rock that is older than the rock around them.

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6
Q

Describe the principle of fossil succession

A

Fossil species follow each other in the rock record in a recognizable and irreversible order. Thus we can use this information to correlate strata over large distances, despite differences in rock type of geologic processes.

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7
Q

What are unconformities

A

Much of geologic time in a given region is not included in the rock record. Theses are times in which the erosion was occurring rather than deposition. We would expect to see rocks of a certain age, but don’t. What we do see is an erosional surface of older rock overlain by younger sediments called an unconformity.

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8
Q

What are the 3 main types of unconformity

A

Angular unconformity
Disconformity
Nonconformity

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9
Q

What is an Angular Unconformity

A

An erosional surface between older layers which have been uplifted and tilted prior to erosion, and younger layers. A different dip angle between the overlying and underlying beds results.

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10
Q

What is a disconformity

A

The older, eroded surface is made of sedimentary layers which have the same orientation as the overlying beds. This type is the most difficult to see in the field and requires a thorough knowledge of local geology, often based on missing fossil sequence.

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11
Q

What is a nonconformity

A

Older, eroded surface is a crystalline rock which is subsequently overlain by sediments. Only contacts between igneous rocks and overlying rocks that are erosional are nonconformities.

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12
Q

What are radioactive isotopes

A

Radioactive isotopes are elements in minerals that are able to tell us how much time has elapsed since the rock was formed. This is because radioactive isotopes are unstable and decay or break down at predictable rates.

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13
Q

What is an isotope

A

An isotope is one of several forms of one element, all having the same number of protons in the nucleus, but differing in the number of neutrons

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14
Q

What is Radiometric dating

A

Radiometric dating is possible because radioactive atoms of some elements are incorporated into the crystal lattice of minerals at the time of their formation. Over time these parent atoms decay and their daughter elements are trapped within the mineral.

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15
Q

What level does radioactive decay occur on

A

Radioactive decay occurs on the atomic level as particles in the nucleus disintegrate, changing the atom into one of a different element and emitting radiation in the process.

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16
Q

What is a half life

A

The half life is the time it takes half a sample of a radioactive isotope to decay. Constant no matter the amount of the isotope. So the time it takes to go from 100% to 50%, is equal to the time it takes to go from 50% to 25%.

17
Q

What is decay curve

A

A decay curve is a simple graph that represents the amount of parent isotope we would expect to find remaining in a mineral or rock after a given period of time has passed.

18
Q

What formula gives the percentage of parent atoms remaining after time n

19
Q

What is the detection limit for most radioactive elements

A

The detection limit for most radioactive elements rarely exceeds five half lives

20
Q

What is the decay of U238

A

U238 -> Pb206
HL = 4.56 BY
Found in Zircons (in granites) and uranitite

21
Q

What is the decay of U235

A

U235 -> Pb207
HL = 704 MY
found in Zircons (in granites), and uranitite

22
Q

What is the decay of K40

A

K40-> Ar40 and Ca40
HL = 1.251 BY
Found in muscovite, biotite, hornblende, K-feldspar, glauconite, volcanic rock

23
Q

What is the decay of Rb87

A

Rb87->Sr87
HL = 48.8 BY
Found in K-mica, K-felspar, Biotite, metamorphic rocks

24
Q

What is the decay of Th230

A

Th230->Pb206
HL = 75 KY
Found in Oceanic Sediments

25
What is the decay of Th232
Th232-> Pb208 HL = 13.9 BY Found in Zircon, Uranitite
26
What is the decay of C14
C14 -> N14 HL = 5,730 Yrs Found in wood, bone, shells
27
What are some other dating methods
Tree-rings, valves, and ice layers are also ways of determining the absolute age of past events.
28
What is Palaeontology
the study of prehistoric animals and plants whose remains are found in sedimentary rocks and described in fossils. To be considered a fossil, all or part of the actual organisms or some trace of its activity must be preserved in the rock
29
What are the Eons of geologic time
Archean (4.7-2.5 BY) Proterozoic (2500-545 MY) (Archean + Proterozoic = Cryptozoic = Hidden life) Phanerozoic (545 MYA - Present) = visible Life
30
What are the Eras of the Phaneroozic
Paleozoic (age of invertebrates) 545-245 MY Mesozoic (Age of reptiles) 245-66 MY Cenozoic (Age of mammals) 66-0 MY
31
What are the Periods of the Paleozoic
Cambrian 545-505 MY Ordovician 505-438 MY Silurian 438-408 MY Devonia 408-360 Carboniferous (360-286) (contains the Mississippian (360-320 MY) and Pennsylvanian (230-286 MY)) Permian 286-245 MY
32
What are the Periods of the Mesozoic
Triassic 245-208 MY Jurassic 208-144 MY Cretaceous 144-66 MY
33
What are the Periods of the Cenozoic
Paleogene 66-24 My Neogene 24-1.6 My (Paleogene + Neogene used to equal the Tertiary) Quaternary 1.6-0 My
34
What are the Epochs of the Paleogene
Paleocene 66-57 MY Eocene 57-37 My Oligocene 37-24 My
35
What are the Epochs of the Neogene
Miocene 24-5.3 My Pliocene 5.3-1.6 My
36
What are the Epochs o f the Quaternary
Pleistocene 1.6-0.01 My Recent 0.01-0 My