rocks_lab1

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Colorado State University, Fort Collins *

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121

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Geology

Date

Dec 6, 2023

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docx

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9

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GEOL 121 Name Section ___________ Rocks 1: Introduction to Rocks and Rock Processes Scientists like to classify things - organisms, planets, stars, clouds, rocks, pretty much anything! Classification is useful because it allows scientists to identify patterns and organize information. In this lab, you will investigate rocks by developing your own classification scheme. You will then learn how scientists classify rocks, and what can be interpreted about a rock’s history based on its classification. Learning Objectives for this Lab: 1. Identifying types of observations that are useful in identifying rocks 2. Categorize rocks based on observable physical characteristics, and explain why classification is an important aspect of science 3. Classify rocks as sedimentary, igneous, or metamorphic, and justify why each rock is included in its classification group 4. Reflect on how their classification schemes compared to the one used by geologists Part 1: Rock Exploration and Differentiation 1. In your groups, observe the samples given to you by your instructor (Sample Group A). Below, brainstorm a list of the observable properties of the rocks that you might use to differentiate them. The properties could be anything that you might see and note about the rock; there is no right or wrong answer here!
GEOL 121 2. Come up with a classification scheme for your rocks; organize your rocks into 3-6 groups. In the table below, list the sample numbers in each group and write a description of the characteristics that define that group. Sample Numbers Description 1,3,12,6,11, Light colored 9,10,8,2,4,5 Dark colored 10,1,11,4,5 Shiny (with crystals) 9,8,12,2,6,3 Dull (without crystals) 3. Discuss your classification scheme with another table group. How are your classmates’ classification schemes similar to and different from the one you came up with? Describe below. Their classifications were more scientifically specific such as effervescence and between coarse and fine grain. Our classifications were broader. 2
GEOL 121 4. Your instructor will give you a new set of samples (Sample Group B). Consider how effective each of the classification schemes your group and your neighbor group \ came up with were in classifying these samples. Then, develop and describe a revised classification scheme based on your discussion and the introduction of the new data (samples). Our classifications are still effective and so were our neighbors’ group. A revised classification scheme we could use could be grain size, layers of grain, and density of the rock. 5. Instead of rocks, imagine that your instructor had asked you to classify fruit- apples, pears, cherries, blueberries, oranges, limes, blackberries, bananas, in order to determine how they are related to each other. a. Would classifying the fruit by color or size help scientists identify and distinguish between different fruit groups? What issues could arise if these characteristics alone were used? E.g., how would this impact the classification of new fruits (pineapple, melons, tomatoes, avocados, etc….) No because if you were to have two apples, one green and one red, they are both apples, but they appear different and can have different tastes. b. Identify classification schemes that could help you divide these fruits into groups that illustrate how they are related to each other. Are there any observable characteristics could you use? Shape/size of the fruit could be an observable characteristic that we could use to classify the fruits. *wait for instructor guidance before beginning Part 2 Part 2: Scientific Classification of Rocks 3
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GEOL 121 1) At this point, your instructor will lead you in a discussion of the accepted scientific classifications for the three primary rock types, and subcategories within each, which is based on how the rocks form. As part of this discussion, fill out the “identifying characteristics” column of the table below. ROCK TYPE SUB-TYPE FORMATION MECHANISM IDENTIFYING CHARACTERISTICS EXAMPLES Igneous Extrusive Forms from the cooling and crystallization of molten rock on the Earth's surface. Interlocking mineral crystals Small/cannot see them Basalt Intrusive Forms from the cooling and crystallization of molten rock underneath the Earth's surface. Large interloc king crystals air bubbles Pegmati te diorite Large interloc Granite 4
GEOL 121 king crystals air bubbles Pegmati te diorite Interlocking mineral crystals Visible to naked eye Sedimentary Detrital Forms from the accumulation and cementation of small particles (sediments) on/near the Earth's surface. Sand feeling – like sandpaper Sandstone Chemical Forms from the precipitation of materials from water on/near the Earth's surface. Minerals that have been precipitated from water May or may not be crystalline Can contain fossils Limestone Metamorphic Foliated Forms when rocks are subjected to some combination of high heat, high pressure, and hot mineral-rich fluids. Interlocking crystals Banded foliation Gneiss Non- Foliated Forms when rocks are subjected to some Large interlocking crystals Not foliated Marble 5
GEOL 121 combination of high heat, high pressure, and hot mineral-rich fluids. 2. Fill out the first three columns of the chart below, classifying each sample from Sample Group A according to the sub-type described on the previous page. Include a description of your reasoning; what observations support your hypothesis? Rock Sample # Hypothesized Classification & Formation Mechanism Supporting Observations & Reasoning Corrected Classification & Formation Mechanism Supporting Observations & Reasoning 1 Igneous intrusive Can see crystals with naked eye 2 Sedimentary chemical Minerals cemented together Sedimentary detrital Cant see the crystals 3 Igneous extrusive Light in weight, no large crystals 4 Metamorphic foliated Banded, visible interlocking crystals 5 Metamorphic nonfoliated Has crystals but no foliation 6 Sedimentary detrital Large particles cemented together 7 Igneous extrusive Small interlocking mineral crystals Igneous intrusive Large interlocking minerals 8 Sedimentary chemical Effervesces 9 Metamorphic foliated Banded but non visible crystals 10 Sedimentary detrital Large crystals cemented together Igneous extrusive Visible crystals, growing in fine grain 11 Igneous intrusive Visible crystals of different types 12 Sedimentary detrital Feels like sandpaper 6
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GEOL 121 Check your answers from question 2 with your instructor before moving on in the lab. Fill out the last two columns on the table based on instructor feedback. 3. Repeat this process with Sample Group B. Rock Sample # Hypothesized Classification & Formation Mechanism Supporting Observations & Reasoning 13 Metamorphic foliated Visible banded foliation 14 Sedimentary detrital Feels like sandpaper, looks like sandstone 15 Sedimentary chemical Effervesces, looks like it has been precipitated 16 Igneous extrusive Small crystals interlocking not visible to naked eye 17 Igneous intrusive Can see large interlocking crystals Part 3: Reflection 1. Reflect on the ease of implementation of the classifications your groups developed in Part 1 of the lab, versus the geologist-defined classifications. a. Which system of classification is easiest to use? Why? 7
GEOL 121 The system we used in part 1 was easy to use because we were able to classify the rocks using readily observable characteristics. b. Which system of classification is the most useful? Justify your answer, including a discussion of what you are defining as “useful” The geologist defined classification system is most useful because it is more rigorous and specific to each rock category, unlike ours which is very broad. c. Explain why classification systems are common across all branches of science, and how scientists may decide what types of observations would be useful to use in classifying rocks, objects, organisms, etc. Because it is more helpful to communicate observation results when using a common but specific classification system. These various systems can confirm multiple scientists findings on the same topic if they are using the same system. 2. Imagine you’re on a trip with a friend and they do not have a background in geology. You both see a rock outcrop and your friend wonders what type of rock the outcrop is made of. a. In a few sentences, how would you describe to your friend what to look for to determine the rock type? Its texture, whether it has visible crystals or not, if there is visible foliation in the rock. b. Give a brief description (a few words) of what observations you would expect your friend to make if the rock is: i. Igneous intrusive: Look for large interlocking crystals ii. Igneous extrusive: small interlocking crystals or no visible crystals iii. Foliated metamorphic: noticeable layers of crystals iv. Non-foliated metamorphic: similar appearance throughout with no visible crystals or layers v. Detrital sedimentary: small noticeable particles/grains / sandpaper feeling vi. Chemical sedimentary: various visible shells/particles cemented together. Looks like it was created by precipitation 8
GEOL 121 3. What aspects of making observations, rock classification, and/or the six rock categories defined in this lab do you feel most confident about? I feel most confident about the more straightforward aspects of identifying rocks such as looking for banding, different layers, and if you can see crystals interlocking together or not. The system of classification developed by our group in Part 1 was relatively easy to use because it relied on readily observable characteristics like color, texture, and crystal presence 4. What aspects of making observations, rock classification, and/or the six rock categories defined in this lab do you still have questions about? How one would be able to do this in the field if you don’t have a magnifying glass or something of that sort. 9
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