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Pseudomorph

Pseudomorph is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Pseudomorph rather than just read about it. In short: In mineralogy, a pseudomorph is a mineral or mineral compound that appears in an atypical form (crystal system), resulting from a substitution process in which the appearance and dimensions remain constant, but the original mineral is replaced by another due to alteration, or chemical substitution, dissolution and refilling, structural changes or incrustation. The name literally means "false form".

Pseudomorph — main illustration
Pseudomorph — illustration

Key takeaways

  • Pseudomorph belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Pseudomorph to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Pseudomorph from memory before moving on to harder problems.

Reference excerpt

In mineralogy, a pseudomorph is a mineral or mineral compound that appears in an atypical form (crystal system), resulting from a substitution process in which the appearance and dimensions remain constant, but the original mineral is replaced by another due to alteration, or chemical substitution, dissolution and refilling, structural changes or incrustation. The name literally means "false form". Terminology for pseudomorphs is "replacer after original", as in brookite after rutile. The term pseudomorphoses was initially used by Haüy.

Substitution pseudomorph

A substitution pseudomorph is a pseudomorph in which one mineral or other material is replaced by another. The original shape of the mineral remains unchanged, but chemical composition, color, hardness, and other properties change to those of the replacing mineral. This happens typically when a mineral of one composition changes by chemical reaction to another of similar composition, retaining the original crystalline shape. It can occur due to the loss of water or through the action of atmospheric agents, such as oxidation, hydration, or carbonation. An example is a change from galena (lead sulfide) to anglesite (lead sulfate) by oxidation. Pyrite crystals transformed into limonite, a compact mixture of iron oxides where goethite generally predominates, are common. In some cases, only partial replacement occurs. The resulting pseudomorph may contain an unaltered core of galena surrounded by anglesite that has the cubic crystal shape of galena.

Infiltration pseudomorph An example of this process is the replacement of wood by silica (quartz or opal) to form petrified wood in which the substitution may be so perfect as to retain the original cellular structure of the wood. An example of mineral-to-mineral substitution is replacement of aragonite twin crystals by native copper, as occurs at the Corocoro United Copper Mines of Coro Coro, Bolivia.

Paramorph

A paramorph (also called allomorph) is a mineral changed on the molecular level only when the structure of a mineral transitions to a more stable polymorph. It has the same chemical composition, but with a different structure. For example, the cubic form of silver sulfide, argentite, does not actually exist below 173°C, and all are pseudomorphized into the monoclinic mineral acanthite. When the structure is very different, as in the aragonite and calcite, the unstable mineral can remains indefinitely in a metastable form, although transformation can occur under some conditions. Usually, the mineral looks identical to the original, unaltered form.

Epimorph and incrustation pseudomorph An incrustation pseudomorph, also called epimorph, results from a process by which a mineral is coated by another and the encased mineral dissolves. The encasing mineral remains, and retains the shape of the original mineral or material. Alternatively, another mineral may fill the space (the mold) previously occupied by some other mineral or material. Examples of quartz epimorph after calcite are found in the La Viesca Mine, Siero (Asturias), Spain.

In other fields Pseudomorphs are also common in paleontology. Fossils are often formed by pseudomorphic replacement of the remains by mineral matter. Examples include petrified wood and pyritized gastropod shells. In biology, a pseudomorph is a cloud of mucus-rich ink released by many species of cephalopod. The name refers to the similarity in appearance between the cephalopod that released it and the cloud itself, in this context meaning literally "false body". This behaviour often allows the cephalopod to escape from predation unharmed, and is often performed as part of what is known as the blanch-ink-jet maneuver. In philosophy, the concept of pseudomorphosis was used by the German philosopher Oswald Spengler to describe how the forms of an older, more widely dispersed culture affect the expression of forms of a younger, emerging culture. The latter develop into forms that are fundamentally alien to the culture's own world-feeling and thereby prevent it from fully developing its own self-consciousness. In archaeology, organic pseudomorphs are impressions of organic material that can accumulate on the surface of metal artifacts as they corrode. They may occur when metal artifacts are buried in contact with organics under damp soil.

See also

Polymorphism (materials science)

References

Dana's Manual of Mineralogy by Cornelis S. Hurlbut, Eighteenth Edition (1971, John Wiley & Sons, Inc.) ISBN 0-471-42225-8

Illustrations

Pseudomorph: Pseudomorph of goethite after pyrite
Pseudomorph of goethite after pyrite
Pseudomorph: Silica pseudomorph after gypsum crystals and silicified serpulid polychaete tubes
Silica pseudomorph after gypsum crystals and silicified serpulid polychaete tubes
Pseudomorph: Native copper pseudomorph after aragonite, with red cuprite and green malachite alteration
Native copper pseudomorph after aragonite, with red cuprite and green malachite alteration
Pseudomorph: Cubic crystals of argentite transformed into acanthite (monoclinic), without any external visible change. Specimen from the San Juan de Rayas Mine, Guanajuato, Mexico. 3 cm.
Cubic crystals of argentite transformed into acanthite (monoclinic), without any external visible change. Specimen from the San Juan de Rayas Mine, Guanajuato, Mexico. 3 cm.

Worked examples

Example 1 — a first encounter with Pseudomorph

Start with the simplest possible case. Write down what Pseudomorph claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Pseudomorph before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Pseudomorph ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Pseudomorph

In research
Pseudomorph appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Pseudomorph in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Pseudomorph is common in secondary-school and first-year university syllabi. It links to neighbouring topics Mineralogy, so understanding it makes those chapters shorter.
In everyday life
Look for Pseudomorph outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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How to study Pseudomorph in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Pseudomorph means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Pseudomorph out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Pseudomorph in simple terms?

In mineralogy, a pseudomorph is a mineral or mineral compound that appears in an atypical form (crystal system), resulting from a substitution process in which the appearance and dimensions remain constant, but the original mineral is replaced by another due to alteration, or chemical substitution…

Why does Pseudomorph matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Pseudomorph?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Pseudomorph.

Tags

  • Mineralogy

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