SOLID STATE PRESS
← Back to catalog
Minerals: Properties and Identification cover
Coming soon
Coming soon to Amazon
This title is in our publishing queue.
Browse available titles
Earth & Environmental Science

Minerals: Properties and Identification

Mohs Scale, Cleavage, and Crystal Systems — A TLDR Primer

You have a geology lab practical next week, a unit test on earth science minerals, or a parent trying to explain why one rock sparkles and another doesn't — and the textbook chapter is dense, slow, and buried under diagrams you can't interpret without a guide.

**TLDR: Minerals** cuts straight to what you need. This short primer covers the five criteria that define a true mineral (and why ice, glass, and seashells don't always make the cut), the physical properties every geology lab mineral identification workflow depends on — hardness, luster, streak, cleavage, fracture, and density — and how to actually use a dichotomous identification key on an unknown specimen. It also explains the seven crystal systems, the major chemical mineral groups from silicates to sulfides, and why any of this matters beyond the exam room.

Written for US high school and early college students taking Earth Science, Physical Geology, or AP Environmental Science, this guide is short by design. No filler, no re-reading the same idea four ways. Every section leads with the one thing you need to take away, backs it up with concrete examples and worked numbers, and flags the misconceptions students most often get wrong.

If you need a focused earth science exam review for minerals before your next test or lab, pick this up and read it in one sitting.

What you'll learn
  • Define a mineral using the five-part geological criteria and distinguish minerals from rocks, glass, and synthetic materials.
  • Apply the major physical properties — hardness, luster, streak, cleavage, fracture, density, and specific gravity — to identify unknown specimens.
  • Use crystal systems and chemical composition to classify minerals into the major groups (silicates, carbonates, oxides, sulfides, sulfates, halides, native elements).
  • Work through a standard mineral identification key the way a geologist or lab student does on an exam.
  • Recognize why mineral identification matters in geology, resource exploration, and everyday materials.
What's inside
  1. 1. What Counts as a Mineral
    Defines a mineral by the five geological criteria and separates minerals from rocks, glass, ice, and biological materials.
  2. 2. Physical Properties: The Geologist's Toolkit
    Walks through the diagnostic physical properties — hardness, luster, color, streak, cleavage, fracture, density — with how to test each in a lab.
  3. 3. Crystal Systems and Internal Structure
    Explains how atomic arrangement produces crystal habits and the seven crystal systems, and why structure controls properties like cleavage.
  4. 4. Chemical Classification: The Major Mineral Groups
    Organizes minerals by anion chemistry into silicates, carbonates, oxides, sulfides, sulfates, halides, and native elements, with key examples of each.
  5. 5. Working Through an Identification Key
    Demonstrates the practical workflow of identifying an unknown mineral using a dichotomous key and worked specimen examples.
  6. 6. Why Mineral Identification Matters
    Connects mineral ID to economic geology, environmental science, building materials, and the broader rock cycle.
Published by Solid State Press
Minerals: Properties and Identification cover
TLDR STUDY GUIDES

Minerals: Properties and Identification

Mohs Scale, Cleavage, and Crystal Systems — A TLDR Primer
Solid State Press

Contents

  1. 1 What Counts as a Mineral
  2. 2 Physical Properties: The Geologist's Toolkit
  3. 3 Crystal Systems and Internal Structure
  4. 4 Chemical Classification: The Major Mineral Groups
  5. 5 Working Through an Identification Key
  6. 6 Why Mineral Identification Matters
Chapter 1

What Counts as a Mineral

Pick up a piece of quartz, a lump of coal, and a seashell. All three come from the ground. Only one is a mineral. Knowing which — and why — is where geology starts.

Geologists define a mineral by five criteria, and a substance has to meet all five to qualify. Miss even one and it gets a different label. The five are: naturally occurring, inorganic, solid, crystalline, and having a definite chemical composition. Walk through each in turn.

Naturally occurring means the Earth (or another planetary body) made it without human intervention. Synthetic rubies grown in a lab have the same chemistry and crystal structure as natural rubies, but they are not minerals by the geological definition. The distinction matters for classification even when the two materials are physically indistinguishable.

Inorganic means the substance was not produced by a living organism's biological processes. This is where shells and bones get ruled out: they are made of calcium carbonate or calcium phosphate, which are genuine mineral compositions, but the organism built them. Coal fails here too — it is compressed, altered organic matter (ancient plant material). A common misconception is that "inorganic" means "contains no carbon." Actually, a few carbon-bearing compounds do qualify as minerals. Diamond, for example, is pure carbon and is absolutely a mineral, because it forms through geological pressure rather than biological activity.

Solid eliminates liquids and gases. Water in a stream is not a mineral. This leads to the one exception students always ask about: ice. Ice that forms naturally — in a glacier, in permafrost, in a snow crystal — meets every criterion. It is naturally occurring, inorganic, solid, crystalline (water molecules arrange into a hexagonal lattice), and has the definite composition H₂O. Geologists do classify natural ice as a mineral. The water in your glass is not a mineral; the ice in a glacier is.

About This Book

If you're a high school student who needs a solid mineral identification study guide for high school Earth Science or a freshman walking into your first geology lab, this book was written for you. It's also useful if you're prepping for an AP Earth Science exam and want a focused mineral classification guide you can read in one sitting — or if you're a parent or tutor who needs to get up to speed fast.

This primer covers everything you need to know about how to identify minerals in Earth science: the five physical properties every geologist tests first, including hardness, cleavage, and streak, the six crystal systems, and the major chemical mineral groups. Think of it as a compact earth science exam review for minerals and rocks, without the filler. A concise overview with no filler.

Read it straight through once, then work the examples embedded in each section. Finish with the problem set at the end to confirm what stuck.

Keep reading

You've read the first half of Chapter 1. The complete book covers 6 chapters in roughly fifteen pages — readable in one sitting.

Coming soon to Amazon