rocks_lab1
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School
Colorado State University, Fort Collins *
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Course
121
Subject
Geology
Date
Dec 6, 2023
Type
docx
Pages
9
Uploaded by PresidentSwan3772
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.
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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
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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
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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?
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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
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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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