Ternary Diagrams: Practice Problems
Solving Earth Science Problems with Ternary Diagrams

Plotting Data on Ternary Diagrams

Sedimentology: Sediment classification

Sedimentologists have their own classification scheme for sediments that is based on grain size, called the Shepherd Classification (shown at right). The Shepherd Classification is most often applied to sediments with minimal organic components or those found in an offshore environment.

Problem 1: You have taken a core sample of sediment from the Gulf of Mexico and are interested in classifying the sample based on the Shepherd Classification (see ternary at right). You run your sample through a set of sieves to separate them by grain size. After sieving, you weigh the sediments and create a table (shown to the left of the Shepherd Classification diagram). Using that data, how would you classify your sample (what name would you give the sediments) using the Shepherd Classification?


Mineralogy: Plotting pyroxene compositions

Many mineral groups that exhibit solid solution (e.g., feldspar, pyroxene, amphibole, etc.) can be plotted on a ternary diagram with respect to three main components to differentiate between different mineral species.

Problem 2: You have analyzed pyroxene in an igneous rock sample that you collected for your senior thesis. You are interested to know what type of pyroxene is present in your sample, which can give you information about the tectonic setting, pressure, and temperatures at which the igneous rock crystallized. Your chemical data (collected on the electron microprobed) is shown (as weight percent of oxides found in pyroxene) in the table with the figure at right. The diagram in the figure (right) is a ternary diagram that can be used to plot pyroxene compositions.

Note: The white spaces on this diagram do not have any fields labeled. That is because any data that does not plot in the gray areas on this ternary diagram is not a pyroxene.

Determine the type of pyroxene (name) in your igneous rock using the pyroxene diagram and table of oxide compositions shown in the figure above. 

Interpreting Points Plotted on Ternary Diagrams

Petrology: Extracting and interpreting plotted rock compositions


Problem 3. A colleague collected some igneous plutonic (coarse-grained/intrusive) rocks (with no feldspathoid) in a field area for a project you are working on. This colleague has plotted the rocks on the ternary diagram below (also known as the IUGS [International Union of Geological Sciences] or Streckheisen diagram) so that you can classify the rocks. The colleague has also color coded the rocks by age: red circle = oldest; yellow square = middle; and blue triangle = youngest. Based on your colleague's analysis, the rocks collected are classified as quartz monzonite (red, oldest), granodiorite (yellow), and granite (blue, youngest).

You are interested in better characterizing the mineral composition of these rocks, so you can say something about how the mineralogy evolved during crystallization. As a result, you want to know how much of each mineral on this diagram is present in the collected rocks. Use the information below to determine the relative percentages of minerals.  


Environmental geochemistry: Water quality 


Geochemists often look at ions (or ionic groups) dissolved in freshwater to determine whether the water is safe, the source of the water, or how water chemistry changes spatially and through time. Freshwater commonly contains the dissolved cationsCations are ions, or charged particles with a positive charge. Ca+2, Mg+2, Na+, and K+ and the anions Anions are ions, or charged particles with a negative charge. or anionic groupsAnionic groups are a group of atoms with a negative charge. Cl-, HCO3-, SO4-2. Major ion composition (cations and anions/anionic groups) can be plotted on ternary diagrams to characterize differences in chemistry, safety of the water, and sometimes the source of the water.


Problem 4: Watersheds in ice-free areas of western Greenland get their freshwater from either ice melt (proglacial) or precipitation (nonglacial). Proglacial and nonglacial watersheds have distinct chemical compositions; that is, the anionic compositions are different for each type of water produced. The ternary diagram for differentiating proglacial and nonglacial watersheds is shown in the ternary to the right with samples from proglacial (blue triangles) and nonglacial (red circles) watersheds plotted.

Use these data to answer the following questions:

a) Which anion (Cl-, SO4-2, or HCO3-) is most abundant in proglacial watersheds?

b) Which anion (Cl-, SO4-2, or HCO3-) is most abundant in nonglacial watersheds?

c) How could you use the information above to determine whether water in another watershed is proglacial or nonglacial?


A More Complex Example: Reading and Plotting

Geomorphology: Dune types


There are many variables that can influence the formation of sand dunes, including topography, climate, humidity, vegetation, availability of sand, and wind strength and direction. The interplay of many of these variables produces different shapes and forms of sand dunes. Geomorphologists use the ternary diagram below to characterize the relationship of dune forms (morphology), vegetative cover, supply of sand, and the strength of the wind.

Problem 5: The photo of the dunes shown in the left portion of the figure below was taken in Oregon Dunes National Recreation Area. In the area near the coastal forest, the interplay of variables that control dune shape is reflected by the location of the blue dot on the dune morphology diagram on the right side of the diagram below. Given the placement of the blue dot, most of the dunes near the coastal forest in Oregon Dunes are classified as parabolic dunes. Your first job is to determine the conditions that produce the parabolic dunes shown in the photo by determining the proportions of the end-members.

Additionally, geomorphologists might want to know how changing one variable might alter the types of dunes that would be present, and so might consider questions like: what would happen if we logged the coastal forest (and reduced vegetation)? So your second job is to plot a new point that reflects reduced vegetation (more information in the question below). Let's use the dune morphology diagram to think about both the conditions that are currently present (the blue dot) and what might happen if we changed the amount of vegetation.

This question involves interpreting the plotted blue point, and plotting a new point that reflects less vegetation. So, the steps outlined below are not exactly what we've been using above. The steps are notated with "interpreting" and "plotting" so that you know where those steps come from.

Next Steps

TAKE THE QUIZ!!  

I think I'm competent with ternary diagrams and I am ready to take the quiz! This link takes you to WAMAP. If your instructor has not given you instructions about WAMAP, you may not have to take the quiz.


Or you can go back to the Ternary Diagrams explanation page.