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Hayford ellipsoid

Hayford ellipsoid is a physics 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 Hayford ellipsoid rather than just read about it. In short: In geodesy, the Hayford ellipsoid is a reference ellipsoid named after the American geodesist John Fillmore Hayford (1868–1925), which was introduced in 1910. The Hayford ellipsoid was also referred to as the International ellipsoid 1924 after it had been adopted by the International Union of Geodesy and Geophysics IUGG in 1924, and was recommended for use all over the world.

Key takeaways

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

Reference excerpt

In geodesy, the Hayford ellipsoid is a reference ellipsoid named after the American geodesist John Fillmore Hayford (1868–1925), which was introduced in 1910. The Hayford ellipsoid was also referred to as the International ellipsoid 1924 after it had been adopted by the International Union of Geodesy and Geophysics IUGG in 1924, and was recommended for use all over the world. Many countries retained their previous ellipsoids. The Hayford ellipsoid is defined by its semi-major axis a = 6378388.000 m and its flattening f = 1:297.00. Unlike some of its predecessors, such as the Bessel ellipsoid (a = 6377397 m, f = 1:299.15), which was a European ellipsoid, the Hayford ellipsoid also included measurements from North America, as well as other continents (to a lesser extent). It also included isostatic measurements to reduce plumbline divergences. Hayfords ellipsoid did not reach the accuracy of Helmert's ellipsoid published 1906 (a = 6378200 m, f = 1:298.3). It has since been replaced as the "International ellipsoid" by the newer Lucerne ellipsoid (1967) and GRS 80 (1980).

See also Earth ellipsoid

Sources Defense Mapping Agency: Geodesy for the layman, 1983, p. 8 [1]

Worked examples

Example 1 — a first encounter with Hayford ellipsoid

Start with the simplest possible case. Write down what Hayford ellipsoid claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In physics, 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 Hayford ellipsoid 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 Hayford ellipsoid 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 Hayford ellipsoid

In research
Hayford ellipsoid appears in physics 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 Hayford ellipsoid 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
Hayford ellipsoid is common in secondary-school and first-year university syllabi. It links to neighbouring topics Ellipsoids, Geodesy, Geodesy stubs, so understanding it makes those chapters shorter.
In everyday life
Look for Hayford ellipsoid 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 Hayford ellipsoid in 20 minutes

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

Frequently asked questions

What is Hayford ellipsoid in simple terms?

In geodesy, the Hayford ellipsoid is a reference ellipsoid named after the American geodesist John Fillmore Hayford (1868–1925), which was introduced in 1910. The Hayford ellipsoid was also referred to as the International ellipsoid 1924 after it had been adopted by the International Union of Geode…

Why does Hayford ellipsoid matter?

Because it connects several physics 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 Hayford ellipsoid?

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 Hayford ellipsoid.

Tags

  • Ellipsoids
  • Geodesy
  • Geodesy stubs
  • Geophysics

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