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Introduction to
Field Geology
CHAPTER
1
I
t is late morning on a crystal clear day in the Livingstone Range of the Canadian
Rockies, and you have traversed uphill over the past several hours through a
sequence of well-bedded sedimentary units. You have determined that you are
moving up section through the units towards younger strata, and that the layers all
dip in the same direction. As you catch your breath at the top of a ridge and admire
the view, you notice that the dip of the layers has reversed. A great discussion
ensues between the members of your field party concerning possible reasons for
the dip reversal (Figure 1.1). What is going on geologically? Is there a fold? Have
you crossed a fault? Can you constrain the timing of the deformational event that
caused the dip reversal? Many ideas are suggested to account for the dip reversal,
and there is no consensus. How, then, do you resolve the problem? After some dis-
cussion, the group concludes that there are several feasible interpretations, and
several possible directions to travel to sort out the fold versus fault question. After
a snack, you and your mapping partner set off in one direction, while other map-
ping teams head off on other routes to see if they can resolve the problem.*
The previous example highlights the use of the scientific method to solve field
problems. You make careful observations of geologic relationships, record them
accurately in your field notebook, develop ideas (hypotheses) about the stratigra-
phy and structure of an area, and set about testing those ideas. Finally, you must
create a geologic map that accurately portrays your observational data and your
resulting interpretations.
Now imagine that you have been hired for the summer as a geological field
assistant. This will likely be your first job in geology, and you are understandably
anxious about what challenges await you over the summer. You have completed a
couple of years towards a university degree in geology. A fundamental course back-
ground in geology has prepared you for this summer job. If you perform well,
* If you are wondering how the problem in the Livingstone Range was resolved, further observations
and measurements demonstrated that the dip reversal was due to the presence of a syncline.
CHAPTER 1 Introduction to Field Geology
2
you might even be asked to stay on part-time with your
employer over the university year to continue working
on the project. Certainly, a period of experience working
in the field will make you much more marketable in the
future. But what will you do every day in the field? What
will be expected of you? This book will help you to
answer those questions.
It is difficult to describe a typical day in the field
because there is such a range of possible projects to be
involved in, all with different objectives. On any given
day you might hike a great distance, moving up and
down over mountains, or you could be delivered direct-
ly to a targeted area by a helicopter. You might create a
geologic map by measuring strikes and dips in folded
layers and plotting geologic contacts, or use an existing
geologic map to locate and sample rocks or sediments
for chemical analysis. There may be logistical challenges
associated with the weather, terrain, or wildlife. In the
evening, you will be reviewing what you did that day,
updating your map and notes, perhaps packaging sam-
ples for shipping, and discussing your observations and
questions with other geologists, as well as preparing for
the next day in the field.
The main focus of this book is on standard methods of
doing geology in the field, including digital techniques
used during field work and for map production. In addi-
tion, there is brief coverage of several subsurface tech-
niques that supplement traditional mapping methods.
WHAT IS FIELD GEOLOGY AND
WHY IS IT IMPORTANT?
Field geology involves integrating spatial, descriptive,
structural, petrologic, and temporal data to understand
the geological makeup and history of an area. Geologic
maps, cross sections, and written reports of an area are
the tangible results of this synthesis. Many field geology
projects focus primarily on making geologic maps.
However, other field tasks include sampling of rock types
for specific reasons (e.g., elemental analysis, geochronol-
ogy, fossil identification), measuring the orientation of
particular structures in an area, or describing the core at
a drill site.
Geologic maps are used to guide the search for min-
eral and energy resources, to assess and mitigate poten-
tial natural hazards, and to assist in land use planning.
A geologic map is the clearest and most concise way to
communicate geologic information about a portion of
Earth’s surface; it represents an interpretation by the
author(s), based on data available at the time of publi-
cation, as to the nature of and spatial distribution of rock
units in an area. Standardized symbols, patterns, and
colours are used to depict rock units, their ages, struc-
tures, and important localities, such as fossil and miner-
al occurrences. Any cross sections and geological reports
that accompany a geologic map represent additional
ways of presenting geologic data and interpretations.
Figure 1-1
Discussing a field geology problem in the Livingstone Range, Canadian Rockies.
Field data are commonly incomplete, and can be
interpreted in more than one way. Taking the purpose of
a mapping project, the budget, and the time allotted to
the project into account, you have to come up with your
best interpretation of the geology based on available
data, and you must trust your own observations and con-
clusions. In some cases, there is no single correct answer
to a field problem. Successful completion of field proj-
ects builds self-esteem, decision-making capability, and
other professional skills. All geoscientists, even experi-
mentalists and theoreticians, need to have some basic
field geology experience.
WHAT MAKES A SUCCESSFUL
FIELD GEOLOGIST?
Table 1.1 lists some of the attributes that government
geological surveys, mineral exploration companies, oil
and gas exploration companies, and environmental and
engineering consulting firms seek in a potential field
geologist.
A successful field geologist is a multi-tasking “jack of
all trades” who has a firm grasp of geological principles,
but also has a number of supplementary skills, such as
being well-organized, possessing common sense, and hav-
ing the ability to maintain a positive attitude in numerous
situations. He or she realizes that thorough preparation
before a project commences, including becoming famil-
iar with previous work in the area and talking to others
who have worked there, is as important as doing the field
work. A field geologist must have excellent observational
skills, have the ability to take accurate measurements and
estimate lengths and quantities, and have at least some
background in petrology and mineralogy, structural
geology, geomorphology, stratigraphy, and paleontology.
The ability to translate a three-dimensional representa-
tion of map data into a cross section and the capacity to
write technical reports are also vital parts of a field geolo-
gist’s repertoire.
Digital maps and associated databases that store large
amounts of geological data in layers (see Chapter 12) are
now standard in the professional workplace, and make it
3
Introduction to Field Geology CHAPTER 1
How to read a topographic map or air photo and locate yourself
Pace and compass skills
Use of Brunton or Silva compass for measuring linear and planar structures
How to locate by compass resection
Use of portable GPS receivers, and knowledge of their limitations
Know how to locate and plot geologic data accurately on a geologic map or air photo
Ability to recognize and measure sedimentary structures, structural features (folds, faults — sense of movement,
lineations, foliations; use of stereonet)
How to measure a stratigraphic section (use of Jacob’s staff or pogo stick)
Rock identification skills (hand sample and thin section; fresh and altered rocks; mineralized assemblages)
Ability to take organized, coherent, and legible notes
Ability to collect properly trimmed rock and fossil specimens; ability to recognize the appropriate rock to sample
depending on the purpose (e.g., microfossil age determination, radiometric age determination — which
accessory minerals for which dating technique, alteration assemblages)
Ability to visualize and think in three dimensions
Some familiarity with mapping software, but no particular programs as they evolve so rapidly; we will teach you
our system
Ability to independently plan, execute, and accurately plot the results of a traverse
Ability to synthesize data into the big picture; to recognize what are the most important geological observations
in an area, depending on the problem to be solved
Ability to write reports in a timely manner; write reports that are complete yet concise
Field safety
Have a positive attitude (every day, in all conditions, on all projects)
Based on a survey of government, industry, and consulting firms who hire field geologists conducted by M.L. Bevier in Vancouver, British Columbia, 1994.
Table 1.1
WHAT EMPLOYERS WANT YOU TO KNOW ABOUT FIELD GEOLOGY
CHAPTER SUMMARY
Field geology can be a lot of hard work, but it is satisfy-
ing to use a wide range of geologic knowledge and skills
to solve field problems. Working in the field provides
opportunities to use and integrate knowledge from many
sub-disciplines in geology.
You are encouraged to take every possible opportu-
nity to increase your field experience and skills, and to
expand and enhance your abilities to make and inter-
pret geologic maps. The ability to solve field problems is
fundamental to a career as a geoscientist. Work safely,
and be a good representative for your profession.
4 CHAPTER 1 Introduction to Field Geology
possible for anyone to create derivative or thematic maps
by selectively querying a database. Today’s student needs
to be able to integrate traditional mapping techniques
with digital data capture and manipulation. However,
the employer responses listed in Table 1.1 suggest that
your ability to rise to the particular challenges of a spe-
cific field project, be they scientific, personal, or logisti-
cal, is more important to employers than the fact that
you are particularly familiar with a specific computer
mapping program that might be superseded in the near
future (although that skill will be a bonus).
Heath (2000, 2002) surveyed geoscience employers
for the most important technical and non-technical skills
that they want to have in their employees. Results of a
similar survey, specifically applicable to the petroleum
geology industry, are available on line at http://www.
aapg.org/education/vgp/survey.cfm.
HOW DO YOU LEARN FIELD
GEOLOGY?
To be a successful field geologist, you must gain practical
experience in a variety of rock assemblages, terrains, and
climates. There is great satisfaction involved in produc-
ing a map that shows the distribution of rock units and
structures in an area, especially after you have hiked over
most of it. Field work can be an exasperating business —
it is normal to be frustrated on some occasions because
there is not necessarily a simple answer to a field prob-
lem. There is only your best interpretation, based on
available data and your geologic knowledge.
The major change in field geology over the 1990s and
into the 21st century is the increased use of digital meth-
ods for recording data, producing geologic maps, and
selectively querying map data, but geologists continue to
traverse, describe strata, measure structures, and enjoy (or
endure) the weather and the terrain. A good geologic map
still depends mainly on the skills of the field geologist who
makes it, and not on flashy graphics or presentation.
For background, you need a combination of specific
courses in sub-disciplines of geology, such as mineralogy,
petrology, structural geology, and geomorphology, but
you must also have basic outdoor skills and a lot of
common sense. Above all, you need to be comfortable
working with incomplete data sets because a successful
field geologist is a generalist who can synthesize a vast
amount of seemingly disparate data into a coherent and
reasonable geological interpretation of an area.
Your first geologic maps are unlikely to be works of
art. You may have gaps in your data that you do not
know how to deal with, but you will still have to make
geologically reasonable interpretations that are consis-
tent with available data to finish your map by a deadline.
With more and varied experience, and critiques from
mentors, your skills at describing rocks and field rela-
tionships, at measuring structures, and at interpreting
complex data sets will improve, and so will the geologic
maps that you generate.
FIELD SAFETY AND ETIQUETTE
Heat exhaustion, a serious cut requiring stitches,
influenza, an infected spider bite, and a twisted ankle —
these are examples of maladies suffered by students in
the field that have necessitated visits to the emergency
ward. Students have been killed in the field by slipping
off the tops of cliffs or by drowning in rivers and lakes.
Vehicle accidents while travelling to and from the field
have also caused injury and loss of life. Although you
may not be able to avoid every emergency, many field
mishaps can be prevented with careful planning and
attention to safety procedures (Appendix A). These pro-
cedures cover field work, camp life, and travel to and
from a field area, and should be read in detail. Adhering
to them will make field work a safe and enjoyable expe-
rience for all involved.
Distinct from safety but just as important is field
etiquette, which includes topics such as environmental
impact, personal behaviour, obtaining permission to
access private property, and proper field sanitation
(Appendix B). Always remember that you are an ambas-
sador for the profession every time that you go into the
field, and act accordingly.

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An Introduction To Field Geology

  • 1. Introduction to Field Geology CHAPTER 1 I t is late morning on a crystal clear day in the Livingstone Range of the Canadian Rockies, and you have traversed uphill over the past several hours through a sequence of well-bedded sedimentary units. You have determined that you are moving up section through the units towards younger strata, and that the layers all dip in the same direction. As you catch your breath at the top of a ridge and admire the view, you notice that the dip of the layers has reversed. A great discussion ensues between the members of your field party concerning possible reasons for the dip reversal (Figure 1.1). What is going on geologically? Is there a fold? Have you crossed a fault? Can you constrain the timing of the deformational event that caused the dip reversal? Many ideas are suggested to account for the dip reversal, and there is no consensus. How, then, do you resolve the problem? After some dis- cussion, the group concludes that there are several feasible interpretations, and several possible directions to travel to sort out the fold versus fault question. After a snack, you and your mapping partner set off in one direction, while other map- ping teams head off on other routes to see if they can resolve the problem.* The previous example highlights the use of the scientific method to solve field problems. You make careful observations of geologic relationships, record them accurately in your field notebook, develop ideas (hypotheses) about the stratigra- phy and structure of an area, and set about testing those ideas. Finally, you must create a geologic map that accurately portrays your observational data and your resulting interpretations. Now imagine that you have been hired for the summer as a geological field assistant. This will likely be your first job in geology, and you are understandably anxious about what challenges await you over the summer. You have completed a couple of years towards a university degree in geology. A fundamental course back- ground in geology has prepared you for this summer job. If you perform well, * If you are wondering how the problem in the Livingstone Range was resolved, further observations and measurements demonstrated that the dip reversal was due to the presence of a syncline.
  • 2. CHAPTER 1 Introduction to Field Geology 2 you might even be asked to stay on part-time with your employer over the university year to continue working on the project. Certainly, a period of experience working in the field will make you much more marketable in the future. But what will you do every day in the field? What will be expected of you? This book will help you to answer those questions. It is difficult to describe a typical day in the field because there is such a range of possible projects to be involved in, all with different objectives. On any given day you might hike a great distance, moving up and down over mountains, or you could be delivered direct- ly to a targeted area by a helicopter. You might create a geologic map by measuring strikes and dips in folded layers and plotting geologic contacts, or use an existing geologic map to locate and sample rocks or sediments for chemical analysis. There may be logistical challenges associated with the weather, terrain, or wildlife. In the evening, you will be reviewing what you did that day, updating your map and notes, perhaps packaging sam- ples for shipping, and discussing your observations and questions with other geologists, as well as preparing for the next day in the field. The main focus of this book is on standard methods of doing geology in the field, including digital techniques used during field work and for map production. In addi- tion, there is brief coverage of several subsurface tech- niques that supplement traditional mapping methods. WHAT IS FIELD GEOLOGY AND WHY IS IT IMPORTANT? Field geology involves integrating spatial, descriptive, structural, petrologic, and temporal data to understand the geological makeup and history of an area. Geologic maps, cross sections, and written reports of an area are the tangible results of this synthesis. Many field geology projects focus primarily on making geologic maps. However, other field tasks include sampling of rock types for specific reasons (e.g., elemental analysis, geochronol- ogy, fossil identification), measuring the orientation of particular structures in an area, or describing the core at a drill site. Geologic maps are used to guide the search for min- eral and energy resources, to assess and mitigate poten- tial natural hazards, and to assist in land use planning. A geologic map is the clearest and most concise way to communicate geologic information about a portion of Earth’s surface; it represents an interpretation by the author(s), based on data available at the time of publi- cation, as to the nature of and spatial distribution of rock units in an area. Standardized symbols, patterns, and colours are used to depict rock units, their ages, struc- tures, and important localities, such as fossil and miner- al occurrences. Any cross sections and geological reports that accompany a geologic map represent additional ways of presenting geologic data and interpretations. Figure 1-1 Discussing a field geology problem in the Livingstone Range, Canadian Rockies.
  • 3. Field data are commonly incomplete, and can be interpreted in more than one way. Taking the purpose of a mapping project, the budget, and the time allotted to the project into account, you have to come up with your best interpretation of the geology based on available data, and you must trust your own observations and con- clusions. In some cases, there is no single correct answer to a field problem. Successful completion of field proj- ects builds self-esteem, decision-making capability, and other professional skills. All geoscientists, even experi- mentalists and theoreticians, need to have some basic field geology experience. WHAT MAKES A SUCCESSFUL FIELD GEOLOGIST? Table 1.1 lists some of the attributes that government geological surveys, mineral exploration companies, oil and gas exploration companies, and environmental and engineering consulting firms seek in a potential field geologist. A successful field geologist is a multi-tasking “jack of all trades” who has a firm grasp of geological principles, but also has a number of supplementary skills, such as being well-organized, possessing common sense, and hav- ing the ability to maintain a positive attitude in numerous situations. He or she realizes that thorough preparation before a project commences, including becoming famil- iar with previous work in the area and talking to others who have worked there, is as important as doing the field work. A field geologist must have excellent observational skills, have the ability to take accurate measurements and estimate lengths and quantities, and have at least some background in petrology and mineralogy, structural geology, geomorphology, stratigraphy, and paleontology. The ability to translate a three-dimensional representa- tion of map data into a cross section and the capacity to write technical reports are also vital parts of a field geolo- gist’s repertoire. Digital maps and associated databases that store large amounts of geological data in layers (see Chapter 12) are now standard in the professional workplace, and make it 3 Introduction to Field Geology CHAPTER 1 How to read a topographic map or air photo and locate yourself Pace and compass skills Use of Brunton or Silva compass for measuring linear and planar structures How to locate by compass resection Use of portable GPS receivers, and knowledge of their limitations Know how to locate and plot geologic data accurately on a geologic map or air photo Ability to recognize and measure sedimentary structures, structural features (folds, faults — sense of movement, lineations, foliations; use of stereonet) How to measure a stratigraphic section (use of Jacob’s staff or pogo stick) Rock identification skills (hand sample and thin section; fresh and altered rocks; mineralized assemblages) Ability to take organized, coherent, and legible notes Ability to collect properly trimmed rock and fossil specimens; ability to recognize the appropriate rock to sample depending on the purpose (e.g., microfossil age determination, radiometric age determination — which accessory minerals for which dating technique, alteration assemblages) Ability to visualize and think in three dimensions Some familiarity with mapping software, but no particular programs as they evolve so rapidly; we will teach you our system Ability to independently plan, execute, and accurately plot the results of a traverse Ability to synthesize data into the big picture; to recognize what are the most important geological observations in an area, depending on the problem to be solved Ability to write reports in a timely manner; write reports that are complete yet concise Field safety Have a positive attitude (every day, in all conditions, on all projects) Based on a survey of government, industry, and consulting firms who hire field geologists conducted by M.L. Bevier in Vancouver, British Columbia, 1994. Table 1.1 WHAT EMPLOYERS WANT YOU TO KNOW ABOUT FIELD GEOLOGY
  • 4. CHAPTER SUMMARY Field geology can be a lot of hard work, but it is satisfy- ing to use a wide range of geologic knowledge and skills to solve field problems. Working in the field provides opportunities to use and integrate knowledge from many sub-disciplines in geology. You are encouraged to take every possible opportu- nity to increase your field experience and skills, and to expand and enhance your abilities to make and inter- pret geologic maps. The ability to solve field problems is fundamental to a career as a geoscientist. Work safely, and be a good representative for your profession. 4 CHAPTER 1 Introduction to Field Geology possible for anyone to create derivative or thematic maps by selectively querying a database. Today’s student needs to be able to integrate traditional mapping techniques with digital data capture and manipulation. However, the employer responses listed in Table 1.1 suggest that your ability to rise to the particular challenges of a spe- cific field project, be they scientific, personal, or logisti- cal, is more important to employers than the fact that you are particularly familiar with a specific computer mapping program that might be superseded in the near future (although that skill will be a bonus). Heath (2000, 2002) surveyed geoscience employers for the most important technical and non-technical skills that they want to have in their employees. Results of a similar survey, specifically applicable to the petroleum geology industry, are available on line at http://www. aapg.org/education/vgp/survey.cfm. HOW DO YOU LEARN FIELD GEOLOGY? To be a successful field geologist, you must gain practical experience in a variety of rock assemblages, terrains, and climates. There is great satisfaction involved in produc- ing a map that shows the distribution of rock units and structures in an area, especially after you have hiked over most of it. Field work can be an exasperating business — it is normal to be frustrated on some occasions because there is not necessarily a simple answer to a field prob- lem. There is only your best interpretation, based on available data and your geologic knowledge. The major change in field geology over the 1990s and into the 21st century is the increased use of digital meth- ods for recording data, producing geologic maps, and selectively querying map data, but geologists continue to traverse, describe strata, measure structures, and enjoy (or endure) the weather and the terrain. A good geologic map still depends mainly on the skills of the field geologist who makes it, and not on flashy graphics or presentation. For background, you need a combination of specific courses in sub-disciplines of geology, such as mineralogy, petrology, structural geology, and geomorphology, but you must also have basic outdoor skills and a lot of common sense. Above all, you need to be comfortable working with incomplete data sets because a successful field geologist is a generalist who can synthesize a vast amount of seemingly disparate data into a coherent and reasonable geological interpretation of an area. Your first geologic maps are unlikely to be works of art. You may have gaps in your data that you do not know how to deal with, but you will still have to make geologically reasonable interpretations that are consis- tent with available data to finish your map by a deadline. With more and varied experience, and critiques from mentors, your skills at describing rocks and field rela- tionships, at measuring structures, and at interpreting complex data sets will improve, and so will the geologic maps that you generate. FIELD SAFETY AND ETIQUETTE Heat exhaustion, a serious cut requiring stitches, influenza, an infected spider bite, and a twisted ankle — these are examples of maladies suffered by students in the field that have necessitated visits to the emergency ward. Students have been killed in the field by slipping off the tops of cliffs or by drowning in rivers and lakes. Vehicle accidents while travelling to and from the field have also caused injury and loss of life. Although you may not be able to avoid every emergency, many field mishaps can be prevented with careful planning and attention to safety procedures (Appendix A). These pro- cedures cover field work, camp life, and travel to and from a field area, and should be read in detail. Adhering to them will make field work a safe and enjoyable expe- rience for all involved. Distinct from safety but just as important is field etiquette, which includes topics such as environmental impact, personal behaviour, obtaining permission to access private property, and proper field sanitation (Appendix B). Always remember that you are an ambas- sador for the profession every time that you go into the field, and act accordingly.