1 Cosmology and the Earth
2 Journey to the Center of the Earth
3 Drifting Continents and Spreading Seas
4 The Way the Earth Works: Plate Tectonics
5 Patterns in Nature: Minerals
6 Up from the Inferno: Magma and Igneous Rocks
7 A Surface Veneer: Sediments, Soils, and Sedimentary Rocks
8 Metamorphism: A Process of Change
9 The Wrath of Vulcan: Volcanic Eruptions
10 A Violent Pulse: Earthquakes
11 Crags, Cracks, and Crumples: Crustal Deformations and Mountain Building
12 Deep Time: How Old Is Old?
13 A Biography of Earth
14 Squeezing Power from a Stone: Energy Resources
15 Riches in Rock: Mineral Resources
16 Unsafe Ground: Landslides and Other Mass Movements
17 Streams and Floods: The Geology of Running Water
18 Restless Realm: Oceans and Coasts
19 A Hidden Reserve: Groundwater
20 An Envelope of Gas: Earth’s Atmosphere and Climate
21 Dry Regions: The Geology of Deserts
22 Amazing Ice: Glaciers and Ice Ages
23 Global Change in the Earth System
Previous Chapter Chapter Next Chapter

Organize

Learn

Connect

Norton Gradebook

Instructors now have an easy way to collect students’ online quizzes with the Norton Gradebook without flooding their inboxes with e-mails.

Students can track their online quiz scores by setting up their own Student Gradebook.

Chapter 5: Patterns in Nature: Minerals

Guide to Reading

Reduce Text SizeIncrease Text SizeEmailPrint Page

Although there are about 4,000 recognized minerals, only a few dozen are common on Earth. If you're fortunate enough to be taking this as a lab class or if you have access to a mineral collection, you'll probably find samples of the common minerals. Do look at them as you read along. Nothing beats hands-on experience for mineral identification and appreciation.

Most of Chapter 5 is devoted to the scientific approach to mineral study, but woven throughout the chapter are consumer-type topics:

  • the contributions of Georgius Agricola and Nicholas Steno in the sixteenth and seventeenth centuries
  • the advances in mineralogy made possible by use of optical and electron microscopes and X-ray diffraction equipment
  • the questionable magical powers of crystals
  • the beauty and legends of gemstones (diamonds and more)
  • even the fabled "dilithium crystals" of Star Trek fame (which don't actually exist)
The author begins with a very detailed definition of minerals. This leads quite naturally into a discussion of crystal formation and crystals' unique internal structures, which determine their external shapes and symmetry.

Mineral identification is the next topic. How do you tell one kind from another when there are so many? Fortunately there are few enough common ones that examination of a few physical properties generally allows identification of specimens in either the field or the lab.

Keeping things organized is a challenge when dealing with large numbers of anything. Since minerals are simply chemical elements or compounds formed naturally on Earth, it's logical and useful to study them as chemical groups. Minerals that are single elements are part of the native metals group. Most minerals that are compounds fit into one of the following chemical groups:

  • silicates
  • sulfates
  • oxides
  • halides
  • sulfides
  • carbonates
The chapter leaves many practical questions unanswered, including questions dealing with mankind's use of minerals as resources for manufacturing products and producing energy. These issues are dealt with in Part V: Earth Resources (Chapters 14 and 15). For now the author pursues the fact that minerals are the building blocks of rocks, and the next three chapters deal with the very geologic topics of igneous, sedimentary, and metamorphic rocks.

« Return to Chapter 5 Study Plan