Lab 5 Exercises
The exercises below will guide you through the sedimentary rock samples in Rock Kits 1 and 2. Review the background information presented in Chapters 5.1 to 5.5 before you begin these exercises. You may wish to consult the Rock Classification Tables at the back of this manual as you complete the exercises below.
Tips for Classifying Sedimentary Rocks
- Your first step when examining any sedimentary rock is to determine if its texture is clastic or crystalline.
- If the texture is clastic, next determine the predominant size of the grains by looking closely through your hand lens and using the grain size chart (see Table A in the Rock Classification Tables appendix).
- Next, describe the sorting, and the shape (roundness) of the grains (Figure C in the Rock Classification Tables appendix). Remember that you are not describing the shape or size of the sample, but of the grains within it!
- If the texture is crystalline, test the sample with a drop (only a drop!) of dilute HCl. If the rock reacts with HCl, look carefully to determine what exactly is reacting (e.g., cement between grains of quartz sand? The entire sample of limestone?).
- Quartz grains come in many colours, but always have vitreous lustre.
- Feldspar grains are commonly white or pink in colour, and in very coarse-grained clastic sedimentary rocks, you may even see feldspar grains broken along cleavage planes. Feldspar grains that have been chemically weathered tend to look chalky and dull (see Figure 5.1.4), which can help you differentiate them from quartz grains.
1. Using your hand lens, carefully examine samples R151, R161, R162, and R181 from your Rock Kit to complete the table below. The example provided indicates the level of detail expected of your observations.
| Sample # | Grain Size (mm) | Energy Level | Roundness | Sorting | Composition (grains and cement) | Rock Name |
| Example | 0.5-2 mm (sand) | Moderate | Sub-rounded | Moderately sorted | 65% quartz, 35% rock fragments, calcite cement | Lithic arenite |
| R151 |
|
|
|
|||
| R161 |
|
|
|
|||
| R162 |
|
|
|
|||
| R181 |
|
|
|
2. Are all four samples in the table above chemical or detrital (clastic) in origin? How can you tell?
3. Indicate where on the diagram each of the samples from the table above is most likely to have formed by considering the grain size, roundness, sorting, and composition.
4. Imagine a large granite pluton has been uplifted and exposed at the surface. Imagine that this granite is the source material for samples R161 and R162.
a) List the minerals you would expect to find in this granite, and their typical weathering products.
b) If these two samples originated from the same source material, explain what process(es) are responsible for the key difference(s) between them? Hint: examine your answers in the table above.
5. Examine chemical sedimentary rock samples RI91, R201, R211, R221, R231, R251, R261, R271, and R281. In the table below, name the mineral and chemical sedimentary roc