C
3 —T
G
This chapter provides a detailed explanation of the methods used by geologists in constructing a geologic time scale. The concepts of relative and absolute dating are with clear differentiation among eons, eras, epochs, and ages. Following this section is a discussion of the Paleozoic, Mesozoic, and Cenozoic Eras.
All of the factors that have been used to determine the age of the earth including the evolution of fossils, sediment deposition rate, ocean salinity, cooling rate, and natural radioactivity are discussed.
By reading and completing information within this chapter, you should gain an understanding of the following concepts:

Explain the difference between actual and relative geologic time.

Describe the Divisions of the Geologic Time Table, i.e. eons, eras, periods, epochs, and ages and how this table was developed.

Discuss the relationship between time units and time-rock units.

Discuss the term half-life as it applies to radioactivity.

Describe the various radioactive timekeepers, i.e. uranium-lead, potassium-argon, rubidium-strontium, carbon-14, and fission tracks.

Speak with confidence regarding the 4.6 billion year-old age of the Earth.
I.
II.
Finding the Age of Rocks: Relative Versus Actual Time
A Scale of Geologic Time
A. Overviewing the Time Scale
B. Divisions in the Geologic Time Scale
C. Evolution of the Geologic Time Scale
1. The Cambrian System
2. The Ordovician and Silurian Systems
3. The Devonian System
4. The Carboniferous System (Mississippian and Pennsylvanian)
5. The Permian System
6. The Triassic, Jurassic, and Cretaceous Systems
7. Divisions of the Cenozoic
III. Actual Geologic Time: Clocks in the Rocks
IV. Radioactivity Provides a Way to Date Rocks
V.
VI.
What Occurs When Atoms Decay
A. The Alpha, Beta, and Gamma of Decay
B. Why Radioactivity Lets Us Date Ancient Rocks with Confidence
C. Why Igneous Rocks Give the Most Trustworthy Dates
D. Half-Life
The Principal Radioactive Timekeepers
A. Uranium-Lead Methods
B. The Potassium-Argon Method
C. The Rubidium-Strontium Method
D. How Carbon-14 Enters the Environment
E. How Carbon-14 Dating Works
F. Fission Track Dating Method
VII. How Old is the Earth?

Chapter 3—Time and Geology
(Pages 27 –45) actual geologic dating (28): The actual age, expressed in years, of a geologic material or event. alpha particle (35): A particle equivalent to the nucleus of a helium atom, emitted from an atomic nucleus during radioactive decay.
Archean Eon (28): Pertaining to the division of Precambrian time beginning 3.8 billion years ago and ending 2.5 billion years ago. atom (34): The smallest particle of matter that can exist as a chemical element. atomic mass (34): A quantity essentially equivalent to the number of neutrons plus the number of protons in an atomic nucleus. atomic number (34): The number of protons in the nuclei of atoms of a particular element. An element is thus a substance in which all of the atoms have the same atomic number. bentonite (36): A layer of clay, presumably formed by the alteration of volcanic ash. It is composed essentially of montmorillonite and related minerals of the smectite group. beta particle (35): A charged particle, essentially equivalent to an electron, emitted from an atomic nucleus during radioactive disintegration.
Cambrian System (30): Exposures of Strata in Wales provide a standard section with which rocks elsewhere in Europe and on other continents can be correlated and are known as the Cambrian System by definition. All other sections deposited during the same time as the rocks in Wales are recognized as
Cambrian by comparison to the standard section. The basal unit is 570 million years. The time interval covered is 570 to 505 million years.
Carboniferous System (32): A division of the Paleozoic Era ranging in geologic time from 360 to 286 million years. It is further divided into the Lower Carboniferous (Mississippian in the U.S., covering 361-
320 million years (and the Upper Carboniferous (Pennsylvanian in the U.S., covering 320-286 million years). This system designated strata that included beds of coal in north-central England.
Cenozoic Era (28): The era in which we are now living. It began at 66 million years (basal unit).
Cretaceous System (32): In geological time, the last period of the Mesozoic Era, preceded by the
Jurassic Period and followed by the Tertiary Period; it extended from 144 million years to 65 million years before present. daughter element (35): An element formed by the radioactive decay of another element.
Devonian System (32): Included in the Paleozoic Era and covers geologic time from 408 to 360 million years. It was determined to be a new system based on the fauna that was different from that of the underlying Silurian and overlying Carboniferous Systems. electron (34): A negatively charged particle of very little mass that orbits the nucleus of an atom. element (34): A unique combination of protons, neutrons, and electrons that cannot be broken down by ordinary chemical methods. eon (28): A major division of the geologic time scale. The Phanerozoic Eon comprises all of the geologic periods from the Cambrian to the Holocene. The term is also sometimes used to denote a span of 1 billion years. epoch (28): A chronological subdivision of a geologic period. Rocks deposited or emplaces during an epoch constitute the series for that epoch.

Chapter 3—Time and Geology era (28): A major division of geologic time, divisible into geologic periods. There are three divisions:
Paleozoic Era, Mesozoic Era, and Cenozoic Era. fission tracks (42): Submicroscopic “tunnels” in minerals produced when high-energy particles from the nucleus of uranium are forcible ejected during spontaneous fission. gamma radiation (35): Emission in the radioactive decay process consisting of a form of invisible electromagnetic waves having even shorter wavelengths than X-rays. geochronology (27): The study of time as applied to Earth and planetary history. half-life (38): The time in which one-half of an original amount of a radioactive atoms decays to daughter products.
Holocene Series (32): A term sometimes used to designate the period of time since the last major episode of glaciation. The term is equivalent to Recent and ranges from 10,000-12,000 years ago to present. isotope (35): Variants of mass numbers of atoms of the same substance. Isotopes are two or more varieties of the same element that have the same atomic number and chemical properties but differ in mass numbers because they have a varying number of neutrons in the nucleus.
Jurassic System (32): A division of the Mesozoic Era covering a geologic time span of 208 to 144 million years ago.
Mesozoic Era (28): Continued for about 179 million years during the Phanerozoic Eon covering the time period from 245 to 66 million years. Its basal unit is 245 million years ago.
Mississippian System (32): Division of the Carboniferous System covering 360 to 320 million years ago.
It is equivalent to the English division known as Lower Carboniferous.
Neogene Series (32): A subdivision of the Tertiary Period that encompasses the Miocene and Pliocene epochs.
Ordovician System (32): The second period of the Paleozoic era, above the Cambrian and below the
Silurian, from approximately 500 million to 440 million years ago.
Paleozoic Era (28): The era of geologic time from the end of the Precambrian until the beginning of the
Mesozoic era. parent element (35): An unstable element that changes by radioactive decay into a stable daughter element.
Pennsylvanian System (32): A division of late Paleozoic geologic time, extending from 320 to 280 million years ago, varyingly considered to rank as an independent period or as an epoch of the
Carboniferous period; named for outcrops of coal-bearing rock formation in Pennsylvania. period (28): A subdivision of an era.
Permian System (32): Division of the Paleozoic Era covering geologic time ranging from 286 to 245 million years ago. Named for a Russian province. Fossils were determined to be intermediate between those of the Carboniferous below and the Triassic above.
Phanerozoic Eon (28): The eon of geologic time during which the Earth has been populated by abundant and diverse life. It is subdivided into the Paleozoic, Mesozoic, and Cenozoic eras. The basal unit is 570 (or 544) million years and it continues through the present geologic time.
Pleistocene Series (32): The older of the two epochs of the Quaternary Period, spanning about 1.8 million to 10,000 years ago. It represents the interval of geological time (and rocks accumulated during that time) extending from the end of the Pliocene Epoch (and the end of Tertiary Period) to the start of the

Chapter 3—Time and Geology
Holocene Epoch. It is commonly characterized as an epoch when the Earth entered its most recent phase of widespread glaciation. Also known as the Ice Age.
Precambrian Period (28): Pertaining to all of geologic time and its corresponding rocks before the beginning of the Paleozoic Era.
Proterozoic Eon (28): Refers to the time interval from 2500 to 544 million years ago. proton (34): An elemental particle found in the nuclei of all atoms that has a positive electric charge and a mass similar to that of a neutron. neutron (34): An electrically neutral (uncharged) particle of matter existing along with protons in the atomic nucleus of all elements except the mass 1 isotope of hydrogen. radioactivity (35): The spontaneous emission of a particle from the atomic nucleus, thereby transforming the atom from one element to another. relative geologic dating (27): Dating which involves placing geologic events and the rocks representing those events in the order in which they occurred without reference to actual time or dates measured in years. This method tells which event preceded or followed another event, or which rock mass was older or younger relative to others. series (30): The time-rock term representing the rocks deposited or emplaced during a geologic epoch. A series is a subdivision of a system.
Silurian System (32): System in the Paleozoic Era determined by the studies of fossiliferous strata outcropping in the hills of south Wales. The geologic time interval is 438 to 408 million years ago. stage (30): The time-rock unit equivalent to an age. A stage is a subdivision of a series. system (28): Refers to the actual rock record of a period. time-rock unit (= chronostratigraphic unit), (28): The rocks formed during a particular unit of geologic time. time-unit (=geochronologic unit), (28): Represents increments of time.
Triassic System (32): A division of the Mesozoic Era with a basal unit of 245 million years. Geologic time covered is 245 to 208 million years ago. The term Triassic refers to a threefold division of rocks of this age in Germany.

Chapter 3—Time and Geology
1. The geologic time scale was originally based on a. the succession of fossil assemblages. b. the theory of organic evolution. c. the rock record. d. the absolute age of rocks based on isotope age dates.
2. The dating method that places geologic events in a chronological order as determined from their position in the rock record. a. relative dating b. absolute dating c. isotopic dating d. neutron dating
3. The actural rocks formed or deposited during a specific time interval are called chronostratigraphic units or a. rock interval. c. time-rock units. b. formation. d. time units.
4. The correct order of time stratigraphic units from largest to smallest is a. age, era, epoch, period. c. age, epoch, era, age. b. period, epoch, age, era. d. era, period, epoch, age.
5. The Carboniferous Systems of Europe and Britain correspond to what systems of North America? a. Triassic and Jurassic c. Cretaceous and Tertiary b. Cambrian and Ordovician d. Mississippian and Pennsylvanian
6. The atomic number of an atom is the number of a. protons and neutrons in the nucleus. c. protons in the nucleus. d. electrons in the outer shell. b. neutrons in the nucleus.
7. An alpha particle is composed of a. 2 electrons. c. 2 neutrons, 2 protons. b. 2 neutrons. d. 2 protons, 2 electrons.
8. An element that has the same atomic number, but different atomic weights is an a. ion. c. atom. b. isotope. d. element.
9. The use of radioactive elements has proven successful for determining absolute (Quantitative) ages because a. most have very long half-lives. b. they are easily found in the field. c. they are abundant in the Earth’s crust. d. the rate of decay is constant for a particular element.
10. An isotope is an atom of an element with a. the same atomic number, a different number of electrons, but the same number of neutrons. b. the same atomic number, but different numbers of protons and electrons. c. the same atomic number, the same number of electrons, but a different number of neutrons. d. a different atomic number, but the same number of electrons and neutrons.
11. The type of radioactive decay that involves the emission of a high velocity electron from the nucleus is a. alpha decay. b. beta decay. c. gamma emission. d. electron reflection.

Chapter 3—Time and Geology
12. Three Eons span the time boundaries of the Earth’s history. The three eons from the oldest to youngest are: a. Proterozoic, Archeon, Phanerozoic. b. Archeon, Proterozoic, Phanerozoic. c. Archeon, Phanerozoic, Proterozoic. d. Proterozoic, Archeon, Phanerozoic.
13. The divisions of the Proterozoic Eon from the oldest to youngest given the Earth’s history are: a. Meso-Archeon, Eo-Archeon, Paleo-Archeon, Neo-Archeon. b. Paleo-Archeon, Meso-Archeon, Paleo-Archeon, Eo-Archeon. c. Eo-Archeon, Paleo-Archeon, Meso-Archeon, Neo-Archeon. d. Neo-Archeon, Meso-Archeon, Paleo-Archeon, Eo-Archeon.
14. The following represent time divisions in geology which are inclusive —from largest to smallest the correct order is: a. Era, Eon, Period, Epoch, Age. b. Eon, Era, Period, Epoch, Age. c. Era, Period, Eon, Epoch, Age. d. Eon, Period, Era, Epoch, Age.
15. The eon before the Precambrian a. Phanerozoic. b. Archeon. c. Neo-Archeon. d. Proterozoic.
16. This type of geologic dating tells which event preceded another or which rock mass is older or younger. a. quantitative dating d. relative dating b. uniformitarism c. Isotopic dating e. absolute dating
17. An element having the same atomic number but different atomic weight. a. ion b. atom c. neutron d. proton e. isotope
18. Associated with protons in a nucleus are particles having the same mass as protons; however, when they are electrically neutral they are called a. Isotopes. c. alpha particles. b. electrons. d. neutrons.
19. Which of the following rock source materials are used in the Potassium-Argon method? a. zircon, uraninite b. muscovite, limestone, zircon c. muscovite, hornblende, glauconite d. coralline limestone, muscovite, zircon
20. Which of the following reflects the correct parent isotope to daughter isotope? a. potassium – 40, lead – 206 c. uranium – 238, lead – 206 b. thorium – 232, lead – 208 d. potassium – 40, strontium – 87

Chapter 3—Time and Geology
1. The oldest rocks of our planet that make up the Archean and Proterozoic are collectively referred to as the .
2. The number of protons in the nucleus of an atom establishes its number of positive charges and is called .
3. The new atom formed from another by radioactive decay, is called .
4. When atoms of the same substance have different mass numbers these variations are called
_____________ .
5 Emission in the radioactive decay process, consisting of a form of invisible electromagnetic waves having even shorter wavelengths than X-rays, is called .
6. The radioactive dating method using electron capture (where a proton is transformed into a neutron) and whose half-life is 1251 million years is called method.
7. The method of age dating that is based on the content of radiocarbon, which has a short half-life of
5730, found in a particular rock is .
8. The actual rocks formed or deposited during a specific time interval are called chronostratigraphic units or ____________________ ___________________.
9. The science of determining the age of rocks is called ________________________.
10. The term ________________ ________________ was coined in 1822 for strata that included coal beds in north-central England.
11. The _________________ ____________________ was named in 1834 by a German geologist for the trifold division of rocks of this age in Germany.
12. An atom’s ____________ ________________ approximately equals the sum of the masses of its protons and neutrons.
13. The epoch that represents a subdivision of the Neogene Period and spans from 2 million years to
10-12 thousand years ago is .
14. The system that takes its name from a province in Russia, and the youngest period in the “ancient life” Paleozoic Era is the .
15. The parent isotope Uranium – 235 has a half-life of 704 million years. What is its daughter isotope?
_____________________.

Chapter 3—Time and Geology
1. Eras may be further subdivided into shorter time units called epochs, which in turn can be further subdivided into periods.
2. The rocks of the Cambrian System take their names from the Latin name for Wales.
3. The number of protons in the nucleus of an atom establishes its number of positive charges and is called its atomic number.
4. A beta emission is a form of radioactive decay where an electron is emitted from the nucleus of a radioactive isotope.
5. The Phanerozoic has been divided into three major subdivisions called periods.
6. The daughter Nuclide of Potassium 40 is strontium 87.
7. Fission tracks are formed by the passage of nuclear particles emitted during the spontaneous fission of uranium.
8. The half-life of carbon 14 is 5730 years.
9. Actual geologic dating places geologic events, and the rocks representing those events in sequence.
10. Source materials for Potassium 40 and its daughter isotope Argon 40 would include muscovite, biotite, hornblende, glauconite, potassium, feldspar, and whole volcanic rock.

10. c
11. b
12. b
13. d
14. b
15. a
16. c
17. e
18. d
19. c
20. c
Multiple Choice
1. a
2. a
3. c
4. d
5. d
6. c
7. c
8. b
9. d
Fill Ins
1. Pre Cambrian
2. atomic number
3. daughter element
4. isotopes
5. gamma radiation
6. potassium
7. Carbon 14
8. time rock units
9. geochronology
10. Carboniferous System
11. Triassic System
12. atomic mass
13. Pleistocene
14. Permian
15. Lead 207
Chapter 3—Time and Geology
True/False
1. F
2. T
3. T
4. T
5. F
6. F
7. T
8. T
9. F
10. T

Chapter 3—Time and Geology
FIGURE 3 –2 (p. 30) The Devonshire strata contained a fossil assemblage characteristic of rocks elsewhere in Europe that were superpositionally higher (hence, younger) than those described as Silurian in southern Wales by Murchison.
FIGURE 3 –7 (p. 37) The stratum beneath the ash must be older than 453.7 million years.
FIGURE 3 –10 (p. 38) If a graph were prepared showing how much sand passed through an hourglass in each unit of time, the graph would display an inclined straight line, indicating that the amount of original material lost from the top of the hourglass to the lower half is the same during each unit of time. Because the amount of original radioactive material that is lost diminishes with time, the curve on a graph showing radioactive decay would consist of an inclined concave curve.
FIGURE 3 –11 (p. 39) The age of a rock having a 207
Pb/
206 of 0.15 would be 2.6 billion years old.