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Principle of original horizontality

Principle of original horizontality is a 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 Principle of original horizontality rather than just read about it. In short: The principle of original horizontality states that layers of sediment are originally deposited horizontally under the action of gravity. It is a relative dating technique.

Principle of original horizontality — main illustration
Principle of original horizontality — illustration

Key takeaways

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

Reference excerpt

The principle of original horizontality states that layers of sediment are originally deposited horizontally under the action of gravity. It is a relative dating technique. The principle is important to the analysis of folded and tilted strata. It was first proposed by the Danish geological pioneer Nicholas Steno (1638–1686). From these observations is derived the conclusion that the Earth has not been static and that great forces have been at work over long periods of time, further leading to the conclusions of the science of plate tectonics; that movement and collisions of large plates of the Earth's crust is the cause of folded strata. As one of Steno's Laws, the principle of original horizontality served well in the nascent days of geological science. However, it is now known that not all sedimentary layers are deposited purely horizontally. For instance, coarser grained sediments such as sand may be deposited at angles of up to 15 degrees, held up by the internal friction between grains which prevents them slumping to a lower angle without additional reworking or effort. This is known as the angle of repose, and a prime example is the surface of sand dunes. Similarly, sediments may drape over a pre-existing inclined surface: these sediments are usually deposited conformably to the pre-existing surface. Also, sedimentary beds may pinch out along strike, implying that slight angles existed during their deposition. Thus the principle of original horizontality is widely, but not universally, applicable in the study of sedimentology, stratigraphy, and structural geology.

See also Law of superposition Principle of cross-cutting relationships Principle of faunal succession Principle of lateral continuity

References

Illustrations

Principle of original horizontality illustration
Principle of original horizontality: The Permian through Jurassic stratigraphy of the Colorado Plateau area of southeastern Utah is a great example of Original Horizontality. These strata make up much of the famous prominent rock formations in widely spaced protected areas such as Capitol Reef National Park and Canyonlands National Park. From top to bottom: Rounded tan domes of the Navajo Sandstone, layered red Kayenta Formation, cliff-forming, vertically jointed, red Wingate Sandstone, slope-forming, purplish Chinle Formation, layered, lighter-red Moenkopi Formation, and white, layered Cutler Formation sandstone. Picture from Glen Canyon National Recreation Area, Utah.
The Permian through Jurassic stratigraphy of the Colorado Plateau area of southeastern Utah is a great example of Original Horizontality. These strata make up much of the famous prominent rock formations in widely spaced protected areas such as Capitol Reef National Park and Canyonlands National Park. From top to bottom: Rounded tan domes of the Navajo Sandstone, layered red Kayenta Formation, cliff-forming, vertically jointed, red Wingate Sandstone, slope-forming, purplish Chinle Formation, layered, lighter-red Moenkopi Formation, and white, layered Cutler Formation sandstone. Picture from Glen Canyon National Recreation Area, Utah.
Principle of original horizontality: A stratigraphic section of Ordovician rock exposed in central Tennessee, US. The sediments composing these rocks were formed in an ocean and deposited in horizontal layers.
A stratigraphic section of Ordovician rock exposed in central Tennessee, US. The sediments composing these rocks were formed in an ocean and deposited in horizontal layers.

Worked examples

Example 1 — a first encounter with Principle of original horizontality

Start with the simplest possible case. Write down what Principle of original horizontality claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In 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 Principle of original horizontality 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 Principle of original horizontality 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 Principle of original horizontality

In research
Principle of original horizontality appears in 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 Principle of original horizontality 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
Principle of original horizontality is common in secondary-school and first-year university syllabi. It links to neighbouring topics Stratigraphy, so understanding it makes those chapters shorter.
In everyday life
Look for Principle of original horizontality 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 Principle of original horizontality in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Principle of original horizontality 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 Principle of original horizontality out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Principle of original horizontality in simple terms?

The principle of original horizontality states that layers of sediment are originally deposited horizontally under the action of gravity. It is a relative dating technique.

Why does Principle of original horizontality matter?

Because it connects several 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 Principle of original horizontality?

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 Principle of original horizontality.

Tags

  • Stratigraphy

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