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Lab 2: Minerals - Essentials of Geology | GEOL 1030, Lab Reports of Geology

Material Type: Lab; Class: Essentials of Geology; Subject: Geology; University: Volunteer State Community College; Term: Unknown 1989;

Typology: Lab Reports

Pre 2010

Uploaded on 08/18/2009

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Essentials of Geology (Geol 1030)
Laboratory #2-Minerals
Introduction
Welcome to the quintessential physical geology laboratory! This begins a four session
laboratory in observing, describing, classifying, and learning the Earth’s physical products.
Minerals are the basic materials in geology, most rocks & some fossils are made up of minerals.
If you work during this laboratory you will be able to identify the common rock-forming minerals
for the rest of your life. If you chat with your neighbor and then just try to memorize the
minerals, you will not perform well on the identification exam. That’s right, you will identifying
the minerals and the rocks that are made up of minerals on an exam. There are about 3,500
known minerals and you are responsible for learning the minerals that make up 99% of the
Earth’s crust (page 62 in your textbook explains). Fortunate for you, that is just a handful of
minerals (you are responsible for knowing twelve minerals on the test).
First & Foremost
What is a mineral? If you do not know the five properties required to be a mineral, you
better learn it now and please do not tell your instructor you don’t know. He may have a heart
attack! List the 5 characteristics below:
1. 2.
3. 4.
5.
Is it a mineral, yes or no? Refer to your list above to make sure.
A snowflake____________ coal______________
Table salt ______________ window glass _____________
Petroleum______________ volcanic glass______
How to identify minerals
There are several physical properties of minerals that will be diagnostic in determining
minerals. Learn the process and then select a few of the most important properties that set each
mineral apart from the others. Read pages 68-70 in your text before this lab! You instructor will
walk you through the process on the first mineral. The dichotomous key below is crucial to
learning the minerals, but keep in mind you will not be able to use it on the exam! Consequently,
complete the table at the end of this lab, then circle or highlight the properties that distinguish that
mineral from the others samples that are most like it. The first step in the identification is to
separate the minerals by luster into metallic or non-metallic. Practice with these! Appendix C in
your book may be used as a reference. Here are the ones you are responsible for:
THE DIRTY DOZEN
Orthoclase Plagioclase Quartz Muscovite
Augite Hornblende Biotite Olivine
Calcite Gypsum Galena Magnetite
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Essentials of Geology (Geol 1030)

Laboratory #2-Minerals

Introduction Welcome to the quintessential physical geology laboratory! This begins a four session laboratory in observing, describing, classifying, and learning the Earth’s physical products. Minerals are the basic materials in geology, most rocks & some fossils are made up of minerals. If you work during this laboratory you will be able to identify the common rock-forming minerals for the rest of your life. If you chat with your neighbor and then just try to memorize the minerals, you will not perform well on the identification exam. That’s right, you will identifying the minerals and the rocks that are made up of minerals on an exam. There are about 3, known minerals and you are responsib le for learning the minerals that make up 99% of the Earth’s crust (page 62 in your textbook explains). Fortunate for you, that is just a handful of minerals (you are responsible for knowing twelve minerals on the test).

First & Foremost What is a mineral? If you do not know the five properties required to be a mineral, you better learn it now and please do not tell your instructor you don’t know. He may have a heart attack! List the 5 characteristics below:

Is it a mineral, yes or no? Refer to your list above to make sure.

A snowflake____________ coal______________ Table salt ______________ window glass _____________ Petroleum______________ volcanic glass______

How to identify minerals There are several physical properties of minerals that will be diagnostic in determining minerals. Learn the process and then select a few of the most important properties that set each mineral apart from the others. Read pages 68-70 in your text before this lab! You instructor will walk you through the process on the first mineral. The dichotomous key below is crucial to learning the minerals, but keep in mind you will not be able to use it on the exam! Consequently, complete the table at the end of this lab, then circle or highlight the properties that distinguish that mineral from the others samples that are most like it. The first step in the identification is to separate the minerals by luster into metallic or non-metallic. Practice with these! Appendix C in your book may be used as a reference. Here are the ones you are responsible for: THE DIRTY DOZEN Orthoclase Plagioclase Quartz Muscovite Augite Hornblende Biotite Olivine Calcite Gypsum Galena Magnetite

DICHOTOMOUS KEY TO THE MINERALS

For Use By The GEOLOGY CLASSES at VOLUNTEER STATE COMMUNITY COLLEGE Developed by Mr. R.D. Coleman

1a. Metallic luster (Caution, metallic does not mean shiny!)– (2) 1b. Non-metallic – (8)

2a. Streak black, dark gray or dark green – (3) 2b. Streak not as above – (7)

3a. Hard; will scratch glass – (4) 3b. Soft; will not scratch glass – (5)

4a. Color black, S.G. = 5.2, magnetic – Magnetite 4b. Color of yellow gold, not magnetic – Pyrite

5a. Color brass yellow, cleavage absent – Chalcopyrite 5b. Color gray to black, cleavage usually present – (6)

6a. Perfect cubic cleavage, S.G. = 7.5 – Galena 6b. Cleavage otherwise; softer than fingernail; S.G. 2.2; marks paper – Graphite

7a. Streak reddish; color steel gray; S.G. 5.6 – Specular Hematite 7b. Streak yellow to brown; cleavage evident; S.G. = 4.0 – Sphalerite

8a. Nonmetallic; light colored – (9) 8b. Nonmetallic; dark colored – (25)

9a. Hard, scratches glass – (10) 9b. Soft; will not scratch glass – (15)

10a. Two cleavage planes intersect at 90 degrees – (11) 10b. Cleavage not evident – (12)

11a. Color white to gray; striations on one cleavage plane – Plagioclase (feldspar) 11b. Color white to red; no striations – Orthoclase (Potassium feldspar)

12a. Vitreous (glassy) luster – (13) 12b. Waxy luster – (14)

13a. Olive-green to yellowish; often in granular masses, S.G. = 3.3 – Olivine 13b. Colorless to almost any color; S.G. = 2.6; not granular – Quartz

29a. Color varies; glassy look – Quartz 29b. Greenish; commonly in granular masses – Olivine

30a. Color red, red-brown or brown – Jasper 30b. Color dark gray to black – Flint

31a. No cleavage evident ; earthy luster; streak red; S.G. = 5-6 - Hematite 31b. Shows cleavage; luster not earthy – (32)

32a. Vitreous luster; perfect basal cleavage; streak white to kaki to gray – Biotite 32b. Resinous luster; yellow-brown streak – Sphalerite

Mineral Identification Worksheet Specimen ID (if any)

Luster Hardness Streak Cleavage Other Properties

Most Diagnostic Property

Mineral Name