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Ol Doinyo Eburru

Ol Doinyo Eburru 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 Ol Doinyo Eburru rather than just read about it. In short: Ol Doinyo Eburru is an active complex of volcanoes in the Great Rift Valley, Kenya to the northwest of Lake Naivasha. It is being exploited for geothermal energy.

Ol Doinyo Eburru — main illustration
Ol Doinyo Eburru — illustration

Key takeaways

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

Reference excerpt

Ol Doinyo Eburru is an active complex of volcanoes in the Great Rift Valley, Kenya to the northwest of Lake Naivasha. It is being exploited for geothermal energy. Soysambu Conservancy is located to the north of the massif, between Lake Elmenteita to the east and Lake Nakuru to the west.

Geology Eburru is part of a group of volcanoes in the rift that also includes Suswa, Longonot, Olkaria, Elmenteita and Menengai. It is separated from Olkaria volcano to the south by the Akira plains. In this part of the rift, the eastern margin is covered by trachytic tuffs, often ignimbritic, and some trachytic lavas. The western margin is covered by trachytic and pantelleritic pumice as well as deposits of ash falls ejected from Eburru.

The Eburru massif rises to 980 metres (3,220 ft) above the floor of the rift. It developed in three stages. The products of the first stage, in the west, are now mostly buried apart from small pantelleritic lava outcrops. The second stage formed the 19.5 kilometres (12.1 mi) Waterloo Ridge on the eastern side of the massif. These rocks came from a series of pyroclastic eruptions originating in a fault zone. The third stage created craters, small cones, domes and lava flows. The summit has more than fifty craters with diameters from 200 metres (660 ft) to 1.25 kilometres (4,100 ft). The pumice lapilli and ash beds from these centers covers most of the massif as well as the western shoulder of the rift. The youngest formations are no more than a few hundred years old. The Eburru massif today is ridge-shaped and eroded, with an east–west orientation. The volcanic complex has an area of 470 square kilometres (180 sq mi). There are two summits, Eburru hill and West hill. There are young craters on the eastern part of the ridge. The east flank has rhyolitic domes that were probably created in the Holocene and are still only partly overgrown with vegetation. There are widespread fumaroles in cinder cones and craters along the faults in the massif.

Geothermal development In October 2009 Geothermal Development Associates announced that they had signed a contract with Kenya Electricity Generating Company Limited to design, supply and commission a wellhead geothermal power plant at Eburru. The plant would include a 2.5 MW steam turbine generator manufactured by Elliott Turbomachinery in Jeannette, Pennsylvania. It has been estimated that Eburru could support a 20 MW geothermal power station.

References

Sources

Illustrations

Ol Doinyo Eburru illustration
Ol Doinyo Eburru: Landsat image of Eburru. Lake Naivasha in lower right. Lava flows of the Elmenteita Badlands at the top-center
Landsat image of Eburru. Lake Naivasha in lower right. Lava flows of the Elmenteita Badlands at the top-center

Worked examples

Example 1 — a first encounter with Ol Doinyo Eburru

Start with the simplest possible case. Write down what Ol Doinyo Eburru 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 Ol Doinyo Eburru 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 Ol Doinyo Eburru 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 Ol Doinyo Eburru

In research
Ol Doinyo Eburru 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 Ol Doinyo Eburru 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
Ol Doinyo Eburru is common in secondary-school and first-year university syllabi. It links to neighbouring topics Active volcanoes, Complex volcanoes, Great Rift Valley, so understanding it makes those chapters shorter.
In everyday life
Look for Ol Doinyo Eburru 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 Ol Doinyo Eburru in 20 minutes

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

Frequently asked questions

What is Ol Doinyo Eburru in simple terms?

Ol Doinyo Eburru is an active complex of volcanoes in the Great Rift Valley, Kenya to the northwest of Lake Naivasha. It is being exploited for geothermal energy.

Why does Ol Doinyo Eburru 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 Ol Doinyo Eburru?

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 Ol Doinyo Eburru.

Tags

  • Active volcanoes
  • Complex volcanoes
  • Great Rift Valley
  • Landforms of Rift Valley Province
  • Mountains of Kenya
  • Nakuru County
  • Quaternary Africa
  • Volcanoes of Kenya

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