Free Course Image Structural Geology: Mapping, Stereonets, Stress, Strain, Faults and Folds

Free online courseStructural Geology: Mapping, Stereonets, Stress, Strain, Faults and Folds

Duration of the online course: 5 hours and 31 minutes

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Free structural geology course: mapping, stereonets, stress and strain, Mohr circles, faults and folds, plus maps, cross sections, and subsurface data.

In this free course, learn about

  • Foundations of Structural Geology
  • Orientations, Vectors, Thickness, and Uncertainty
  • Planes in the Field: Three-Point Problem and Map Geometry
  • Geologic Maps, Cross Sections, and Subsurface Interpretation
  • Stereonets and Rotations
  • Strain and Deformation Analysis
  • Stress, Rock Strength, and Failure
  • Faults: Geometry, Kinematics, and Reactivation
  • Folds: Geometry, Classification, and Mechanics

Course Description

Learn how geologists read and build the structural story of the Earth with this free online course in structural geology from the University of Stavanger. Designed for basic education within geography, it connects core concepts with practical workflows used in the field and in the subsurface.

Progress from foundational ideas to hands-on mapping skills, including the orientation of lines and planes, vector thinking, thickness calculations, uncertainty and error propagation, and classic mapping problems such as the three-point problem, outcrop traces, and the rule of Vs. You will also explore geologic maps, cross sections, down-plunge projection, and how to integrate seismic reflection and well data to interpret structures below the surface.

Build confidence with stereonets by plotting planes, lines, poles, and rotations, then move into deformation by developing an intuitive and quantitative grasp of strain. The course introduces measures and mathematics of strain, infinitesimal versus finite strain, and the use of Mohr circles, including ways to estimate strain from deformed markers through geometric methods and Mohr circle approaches.

Extend your understanding to stress and rock deformation, including subsurface stress, Mohr circle derivation and application, experimental deformation, failure envelopes, brittle behavior, and the strength of the crust. Finally, develop a clear framework for analyzing faults and folds, covering subsurface and map-based interpretation, juxtaposition, kinematics and indicators, stress axes, fault classification, reactivation, and the mechanics and classification of folding. By the end, you will have a coherent toolkit for interpreting structural patterns and communicating them through maps and quantitative analysis.

Course content

  • Video class: Lecture 1: Introduction to Structural Geology 04m
  • Exercise: Which three approaches (levels of study) are used in structural geology to analyze deformed rocks?
  • Video class: Lecture 2: Orientation of lines and planes 08m
  • Exercise: In the right-hand rule convention, what is the relationship between strike and dip direction for a plane?
  • Video class: Lecture 3: Lines as vectors 05m
  • Exercise: In a right-handed Cartesian coordinate system used in geology, what does right-handed mean?
  • Video class: Lecture 4: Thickness and depth 04m
  • Exercise: Which statement correctly distinguishes true (stratigraphic) thickness from apparent thickness of a tabular layer?
  • Video class: Lecture 5: Thickness using linear algebra 03m
  • Exercise: After transforming points into the strike–dip–pole (S–D–P) coordinate system, how is bed thickness computed?
  • Video class: Lecture 6: Error propagation 02m
  • Exercise: When two independent, random measurements X and Y are used to compute a result Q, which method should be used to combine their uncertainties?
  • Video class: Lecture 7: The three-point problem 06m
  • Exercise: In the three-point problem, what vector operation is used to calculate a vector normal to the plane defined by three non-colinear points?
  • Video class: Lecture 8: Outcrop trace of a plane 03m
  • Exercise: How can you determine the outcrop trace of a planar surface on a topographic map?
  • Video class: Lecture 9: The rule of V's 04m
  • Exercise: According to the rule of V’s, how does a horizontal rock layer appear on a topographic map when crossing a valley?
  • Video class: Lecture 10: Geologic maps 06m
  • Exercise: Which cross-cutting relationship indicates that the curved contact is an unconformity?
  • Video class: Lecture 11: Cross sections 11m
  • Exercise: When choosing a line of section to display the true geometry of a mapped horizon from structure contours, which orientation is best?
  • Video class: Lecture 12: The down-plunge projection 03m
  • Exercise: In a down-plunge projection for a fold, which plot produces the fold profile plane cross-section after transforming coordinates to the fold coordinate system?
  • Video class: Lecture 13: Seismic reflection data 09m
  • Exercise: In seismic reflection surveys, what is directly measured along the vertical axis before any velocity conversion is applied?
  • Video class: Lecture 14: Well data 04m
  • Exercise: What is the main purpose of a checkshot survey in a well when tying well data to a seismic section?
  • Video class: Lecture 15: The stereonet 06m
  • Exercise: What does a plane passing through the center of the sphere plot as on a stereonet?
  • Video class: Lecture 16: Lines and planes on the stereonet 04m
  • Exercise: When manually plotting a plane on an equal-area stereonet, what is the correct sequence of steps?
  • Video class: Lecture 17: Poles on the stereonet 02m
  • Exercise: On a stereonet, what is the pole to a plane?
  • Video class: Lecture 18: Rotations 04m
  • Exercise: On a stereonet, what changes when you rotate a line 40° clockwise about a vertical axis pointing downward?
  • Video class: Lecture 19: Deformation and strain 07m
  • Exercise: Which statement best describes the difference between continuous and discontinuous strain?
  • Video class: Lecture 20: The measures of strain 05m
  • Exercise: Which relationship between stretch (S) and elongation (e) is correct for a line that changes length from Li to Lf?
  • Video class: Lecture 21: The mathematics of strain 08m
  • Exercise: Which statement correctly matches the transformation with what it computes?
  • Video class: Lecture 22: Infinitesimal and finite strain 12m
  • Video class: Lecture 23: The Mohr Circle for strain 06m
  • Exercise: In a Mohr circle for infinitesimal strain, at what angle to the ε1 direction does maximum shear strain occur?
  • Video class: Lecture 24: The Mohr Circle for finite strain 06m
  • Exercise: In a finite-strain Mohr circle diagram, where do positive angular shear (and shear strain, ) values plot relative to the horizontal axis?
  • Video class: Lecture 25: Strain from deformed markers using geometrical methods 07m
  • Exercise: In the Fry method for estimating strain from particles, what feature in the final plot indicates the strain ellipse?
  • Video class: Lecture 26: Strain from deformed markers using the Mohr Circle 07m
  • Exercise: When constructing a Mohr circle for strain using angular shear (γ′) and λ′ axes, where do lines with positive angular shear plot relative to the horizontal λ′ axis?
  • Video class: Lecture 27: Stress 05m
  • Exercise: In a symmetric stress tensor at a point, how many independent stress components (tractions) are there?
  • Video class: Lecture 28: Stress in the subsurface 11m
  • Exercise: In a vertical borehole, borehole breakouts observed on borehole images are most useful for determining which stress information?
  • Video class: Lecture 29: Derivation of the Mohr Circle for stress 05m
  • Exercise: In Mohr circle for stress (using principal stresses σ1 and σ3), what are the center and radius of the circle?
  • Video class: Lecture 30: Use of the Mohr Circle for stress 10m
  • Exercise: In a Mohr circle for stress, what is the effect of increasing pore fluid pressure (p) on the circle?
  • Video class: Lecture 31: Experimental rock deformation 12m
  • Exercise: In a triaxial rock deformation test, what is typically plotted on the y-axis of the stress–strain curve?
  • Video class: Lecture 32: The failure envelope 09m
  • Exercise: In the Mohr-circle interpretation of failure, why does the shear fracture form at point P2 rather than at P1 (maximum shear stress)?
  • Video class: Lecture 33: The brittle regime 07m
  • Video class: Lecture 34: The strength of the crust 06m
  • Exercise: In the jelly sandwich model of lithospheric strength, what do the bread slices represent?
  • Video class: Lecture 35: Introduction to faults 05m
  • Exercise: In a dip-slip fault, what defines a normal fault versus a reverse fault?
  • Video class: Lecture 36: Faults in subsurface data 08m
  • Exercise: In a vertical well that cuts horizontal strata, which type of fault typically produces a missing stratigraphic section at the fault cut?
  • Video class: Lecture 37: Faults in structure maps 08m
  • Exercise: On a structure map, which measurement is defined as the horizontal distance traced perpendicular to the structure contours of the fault (i.e., along the fault dip direction)?
  • Video class: Lecture 38: Fault juxtaposition 04m
  • Exercise: In fault seal analysis, what defines a juxtaposition seal?
  • Video class: Lecture 39: Fault kinematics 12m
  • Video class: Lecture 40: Fault kinematic indicators 06m
  • Exercise: What do slicken fibers on a fault surface indicate about fault movement?
  • Video class: Lecture 41: T and P axes 04m
  • Exercise: In a T–P axis diagram for a fault with striations, how are the T and P axes positioned relative to the slip direction on the movement (M) plane?
  • Video class: Lecture 42: Dynamic classification of faults 07m
  • Exercise: In Anderson's dynamic classification, which principal stress is vertical in a normal fault regime?
  • Video class: Lecture 43: Faulting and stress magnitudes 06m
  • Exercise: Under frictional equilibrium in the upper crust, which faulting regime generally requires the greatest differential stress (largest Mohr circle) for renewed slip at a given depth?
  • Video class: Lecture 44: Fault reactivation 03m
  • Exercise: How does decreasing the coefficient of friction on a pre-existing fault affect its likelihood of reactivation?
  • Video class: Lecture 45: Introduction to folds 12m
  • Exercise: In a cylindrical fold, what pattern do bedding poles form on a stereonet (Pi diagram)?
  • Video class: Lecture 46: Dip isogons and fold classes 04m
  • Exercise: In Ramsay fold classification, which fold class is defined by parallel dip isogons and is commonly called a similar fold?
  • Video class: Lecture 47: The mechanics of folding 10m
  • Exercise: Which statement best describes flexural shear folding as a kinematic model for class 1B (parallel) folds?
  • Video class: Lecture 48: Folds and minor structures 09m
  • Exercise: In the Hansen slip method, where does the transport (slip) direction of a thrust lie relative to populations of Z (dextral) and S (sinistral) minor folds on a stereonet?

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