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Geology of Africa

Geology of Africa 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 Geology of Africa rather than just read about it. In short: The geology of Africa is varied, complex, and gives rise to the wide variety of landscapes found across the continent. The African continent rests over two main plates.

Geology of Africa — main illustration
Geology of Africa — illustration

Key takeaways

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

Reference excerpt

The geology of Africa is varied, complex, and gives rise to the wide variety of landscapes found across the continent. The African continent rests over two main plates. The African Plate (Nubian Plate), accounting for the whole of north Africa, and the Somali Plate, which accounts for the eastern side of mid and southern Africa. The Somali Plate is moving away from the African Plate in a split from Djibouti in the north, to Eswatini in the south. The parting of these two plates formed the southern part of what used to be known as the Great Rift Valley. In geological terms, the African and Somali plate separation has formed the East African Rift System (EARS), comprising two separate rifts systems - the Eastern Rift Valley, and a western branch known as the Albertine Rift. Two massive domes were formed, the Kenyan dome and the Ethiopian dome (known as the Ethiopian Highlands). The Albertine Rift follows the western edge of the Kenyan dome. This runs from Lake Malawi in the south, up into Lake Rukwa, Lake Tanganyika and Lake Albert in the north, where it ends. The Kenyan dome has the eastern branch of the EARS (known as the Gregory Rift) running through its middle, and contains most of what we historically saw as the Great Rift valley. Lake Victoria lies in the middle of the dome, with the Gregory Rift to the east of it. The Gregory rift has Lake Eyasi & Lake Manyara at its southern end, running north up to the west of Nairobi and continuing on through Kenya to Lake Turkana - which lies between the northern edge of the Kenyan dome and the southern edge of the Ethiopian dome. The Ethiopian dome is split down the middle by the Eastern Rift, formed by the developing plate boundary, and has formed a valley running from Lake Chamo and Lake Abaya in the south, widening through Lake Shala, Lake Ziwa and Lake Koku, until it reaches its widest point some 110 kilometres (68 mi) from Djibouti.

Major geological events Vredefort impact structure

Geological features Central African Shear Zone

Geologists of Africa Maria Wilman Hugo Dummett

Geological maps

See also Category: Geologic groups of Africa Category: Stratigraphy of Africa

References

Works cited Dawson, John Barry (2008). The Gregory rift valley and Neogene-recent volcanoes of northern Tanzania. Geological Society Memoir No. 33. Geological Society of London. ISBN 978-1-86239-267-0. Owiunji, I.; Plumptre, A.J. (2011). "The importance of cloud forest sites in the conservation of endemic and threatened species of the Albertine Rift". Tropical Montane Cloud Forests: Science for Conservation and Management. Cambridge University Press. ISBN 978-0521760355.

Further reading Africa's Top Geological Sites (35th International Geological Congress Commemorative Volume), 2016 ISBN 9781775844488

External links United States Geological Survey maps of the geology of Africa (PDF) Interactive map of the topography of Africa - five selectable sources, including; OpenTopoMap, ESRI Topo & CyclOSM

Illustrations

Geology of Africa: Motion of the Nubian (purple, center) and Somali (green, right) Plates
Motion of the Nubian (purple, center) and Somali (green, right) Plates
Geology of Africa: Central African Shear Zone
Central African Shear Zone
Geology of Africa: 1930s geological map of Africa
1930s geological map of Africa
Geology of Africa illustration
Geology of Africa illustration

Worked examples

Example 1 — a first encounter with Geology of Africa

Start with the simplest possible case. Write down what Geology of Africa 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 Geology of Africa 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 Geology of Africa 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 Geology of Africa

In research
Geology of Africa 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 Geology of Africa 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
Geology of Africa is common in secondary-school and first-year university syllabi. It links to neighbouring topics Africa stubs, Geology of Africa, Regional geology stubs, so understanding it makes those chapters shorter.
In everyday life
Look for Geology of Africa 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 Geology of Africa in 20 minutes

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

Frequently asked questions

What is Geology of Africa in simple terms?

The geology of Africa is varied, complex, and gives rise to the wide variety of landscapes found across the continent. The African continent rests over two main plates.

Why does Geology of Africa 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 Geology of Africa?

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 Geology of Africa.

Tags

  • Africa stubs
  • Geology of Africa
  • Regional geology stubs

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