Assignment 1 - Mineral Identification 10 week-1 (2)
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School
Raritan Valley Community College *
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Course
157
Subject
Geology
Date
Jan 9, 2024
Type
docx
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Uploaded by ProfFlower3801
Assignment 1 – Virtual Mineral
Identification
Introduction
Mineral identification is a necessary skill all geologist must poses. Essentially all modern day materials
(not made from plants) are made with minerals that had to be identified in the field in order to be
extracted, processed, and repurposed as human technology. While you complete the lab, thinGF broader
about each mineral, how did it most likely form? What group does it belong to? What environment
might we find that mineral forming today?
Part 1 - Pre-lab exercise (4 points)
In your own words, provide a definition for the following mineral properties.
Mineral Property
Definition
Color
The hue of the rock (yellow, purple, magenta, etc..)
Streak
The hue of the rock when powdered
Hardness
Resistance to being damaged
Cleavage
Breaking the mineral along the weak spot to get an even split
Crystal Form
The shape of the crystal
Fracture
a broken piece of the mineral not placed along the Cleavage
Luster
Light relfelcted off mineral
Part 2 – Mineral Identification (4 points)
Visit
http://profharwood.x10host.com/GEOL101/Labs/Minerals/index.htm
and read the introductory
instructions. Familiarize yourself with how the virtual lab works by experimenting with a few samples
prior to getting started. Once familiar, use the virtual lab to identify mineral samples and complete the
table located below. (You only need to do the first 12).
Sample
Number
Color
Streak
Hardnes
s
Clea
vage
Crystal Form
Fracture
Luster
Other
Mineral
Name
1
White
White
2
1
none
irregular
non-
metallic
none
Gypsum
2
red brown
white
7
0
none
conhoidal
non-
metallic
none
Garnet
3
yellow/gol
d
gray
6
0
pyrittohedron
irriegular
metallic
magneti
c
pyrite
4
clear
white
7
0
hexagonal
con
non
none
Quartz
5
red brown
white
9
0
hexagonal
conhoidal
non
none
corundum
6
grey
white
6
2
none
irreg
non
none
plagioclas
e
7
grey
grey
6
0
none
irreg
strong
metallic
magneti
c
magnetite
8
green
white
5
1
hex
con
non
none
apatite
9
pink
white
6
2
none
irreg
non
none
orthoclase
10
clear
white
2
3
cubic
con
non
salty
halite
11
clear
white
2
1
none
irreg
non
none
muscovite
12
green
white
7
0
none
con
non
bobe
olivine
Part 3 Post Lab Reflection (12 points)
1.
Pretend you are a professional geologist taking your RVCC student intern on a hunt for bauxite
for the aluminum industry. Describe
in detail
how you would go about training the young intern
while identifying bauxite in the field among other rocks. Remember, in the field, rocks and
minerals weather, become covered in biological material, and or oxidize.
To find bauxite the first step is understanding where it is located, bauxite is located near tropical and
subtropical regions. Looking up geological surveys conducted by government agencies to find
information on the specific place that contains bauxite. Conduct a field survey to look for sign of
weathered rock and use sensing technology like satellite images.
2.
Of the minerals identified in the lab exercise, which are you most likely to find in a dried sea
bed? Explain why each mineral has the possibility to exist in this location AND how you would be
able to tell the difference between them.
Dried sea beds provide exceptional mineral making material beause of the evaporation of water. The
mineral that could be found is halite and gypsum the dissolved water evaporates and the salt form the
crystals. They can appear in different shapes due to impurities.
3.
Reflect on the mineral identification lab, select three minerals that stood out to you. Explain
what critical thinking and data analysis skills you used in order to identify that mineral.
Pyrite, often referred to as "fool's gold," has a brassy yellow color and metallic luster. It forms cubic
crystals and can also appear as irregular masses. One of its key features is its hardness; it scratches easily
and leaves a greenish-black streak when rubbed against a rough surface. Quartz, on the other hand,
comes in a variety of colors and crystal shapes, but it is commonly recognized for its hexagonal prismatic
crystals and a hardness of 7 on the Mohs scale, meaning it can scratch glass. Quartz is also often
transparent or translucent, allowing light to pass through. Halite, or rock salt, typically occurs as colorless
or white cubic crystals. It has a hardness of 2.5 on the Mohs scale and is easily scratched by a fingernail.
A distinctive characteristic of halite is its salty taste; if you were to lick it, it would taste salty, providing a
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quick and unique way to confirm its identity. By paying attention to these specific traits, geologists can
accurately differentiate between pyrite, quartz, and halite in various geological settings.