ArticleslgStudy

earth science

Rootless cone

Rootless cone 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 Rootless cone rather than just read about it. In short: A rootless cone, also formerly called a pseudocrater, is a volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit ("root") which connects below the surface of a planet.

Rootless cone — main illustration
Rootless cone — illustration

Key takeaways

  • Rootless cone 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 Rootless cone to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Rootless cone from memory before moving on to harder problems.

Reference excerpt

A rootless cone, also formerly called a pseudocrater, is a volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit ("root") which connects below the surface of a planet. Rootless cones are formed by steam explosions as flowing hot lava crosses over a wet surface, such as a swamp, a lake, or a pond. The water from the wetland heats up and forms steam underneath the lava. The explosive gases eventually break through the lava surface in a manner similar to a phreatic eruption, and the tephra builds up crater-like forms which can appear very similar to real volcanic craters. Well known examples are found in Iceland such as the craters in the lake Mývatn (Skútustaðagígar), the Rauðhólar in the region of the capital city Reykjavík or the Landbrotshólar of South-Iceland's Katla UNESCO Global Geopark near Kirkjubæjarklaustur. Volcanologists witnessed the formation of a rootless cone for the first time in history during a steam explosion in connection with the first eruption of Eyjafjallajökull in March 2010.

Martian rootless cones Rootless cones have also been discovered in the Athabasca Valles region of Mars, where lava flowed over superheated groundwater in the underlying rocks. Many such rootless cones have been imaged by the HiRISE camera on the Mars Reconnaissance Orbiter (MRO).

See also

Hornito List of rocks on Mars Littoral cone Maar Volcanism of Iceland

References

External links Pseudocraters and Mars (PDF file) Cones and Inflated Lava Flows on Mars video and pictures of the formation of pseudocraters at Eyjafjallajökull 2010

Illustrations

Rootless cone: A rootless cone at Myvatn Lake, Iceland.
A rootless cone at Myvatn Lake, Iceland.
Rootless cone illustration
Rootless cone illustration
Rootless cone illustration
Rootless cone illustration

Worked examples

Example 1 — a first encounter with Rootless cone

Start with the simplest possible case. Write down what Rootless cone 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 Rootless cone 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 Rootless cone 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 Rootless cone

In research
Rootless cone 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 Rootless cone 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
Rootless cone is common in secondary-school and first-year university syllabi. It links to neighbouring topics Volcanic landforms, Volcanoes, Volcanology, so understanding it makes those chapters shorter.
In everyday life
Look for Rootless cone 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.

Affiliate

Preply — study more efficiently by working with a personal tutor. 50% off.

How to study Rootless cone in 20 minutes

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

Frequently asked questions

What is Rootless cone in simple terms?

A rootless cone, also formerly called a pseudocrater, is a volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit ("root") which connects below the surface of a pl…

Why does Rootless cone 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 Rootless cone?

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 Rootless cone.

Tags

  • Volcanic landforms
  • Volcanoes
  • Volcanology

Keep exploring