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Tollmann's bolide hypothesis

Tollmann's bolide hypothesis 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 Tollmann's bolide hypothesis rather than just read about it. In short: Tollmann's bolide hypothesis, proposed by Austrian palaeontologist Edith Kristan-Tollmann and geologist Alexander Tollmann in 1994, holds that one or more bolides struck the Earth around 7640 ± 200 BCE and that a smaller impact occurred around 3150 ± 200 BCE. The hypothesis proposes that the impacts produced catastrophic environmental effects, including megatsunamis penetrating far into the continents.

Tollmann's bolide hypothesis — main illustration
Tollmann's bolide hypothesis — illustration

Key takeaways

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

Reference excerpt

Tollmann's bolide hypothesis, proposed by Austrian palaeontologist Edith Kristan-Tollmann and geologist Alexander Tollmann in 1994, holds that one or more bolides struck the Earth around 7640 ± 200 BCE and that a smaller impact occurred around 3150 ± 200 BCE. The hypothesis proposes that the impacts produced catastrophic environmental effects, including megatsunamis penetrating far into the continents. Quaternary geologists, paleoclimatologists, and planetary geologists specialising in meteorite and comet impacts have rejected the hypothesis. They argue that the evidence offered for it is more readily explained by ordinary geological processes, that many events attributed to the proposed impacts occurred hundreds to thousands of years outside the hypothesised dates, and that there is no credible physical evidence for the continent-scale megatsunamis and environmental devastation that the hypothesis predicts. In particular, acidity spikes in Greenland ice cores cited as impact evidence have been attributed to volcanic eruptions, while Australasian tektites have been dated to about 790,000 years BP, far earlier than the proposed Holocene impacts. Marine sediments cited as evidence of catastrophic flooding can also be explained by post-glacial isostatic depression. The formation of salt lakes and salt flats cited in support of the hypothesis can be explained by evaporation in endorheic basins, and palaeoenvironmental records from North America and elsewhere do not show the widespread ecological disruption or tsunami deposits expected from the proposed megatsunamis.

Scientific evaluation Quaternary geologists, paleoclimatologists, and planetary geologists specialising in meteorite and comet impacts have rejected Tollmann's bolide hypothesis. They reject this hypothesis because:

The evidence offered to support the hypothesis can more readily be explained by more mundane and less dramatic geologic processes Many of the events alleged to be associated with this impact occurred at the wrong time (i.e., many of the events occurred hundreds to thousands of years before or after the hypothesized impacts); and There is a lack of any credible physical evidence for the cataclysmic environmental devastation and characteristic deposits that kilometre-high tsunamis would have created had they actually occurred.

Evidence used by proponents of the Tollmann's bolide hypothesis to argue for catastrophic Holocene extinctions have alternative explanations by more frequently occurring geological processes. The chemical composition and presence of volcanic ash with the specific acidity spikes in the Greenland ice cores shows evidence that they result from volcanic instead of impact origins. Also, the largest acidity spikes found in Antarctica ice cores have been dated to 17,300 to 17,500 BP, which is significantly older than hypothetical Holocene impacts. The formation of modern salt lakes and salt flats is explained by the concentration of salts and other evaporite minerals by the evaporation of water from stream-fed lakes lacking external outlets, called endorheic lakes, which commonly occur in arid climates on both hemispheres on Earth. The composition of the salts and other evaporite minerals found in these lakes is consistent with their precipitation from dissolved material continually carried into the lakes by rivers and streams and subsequent concentration by evaporation, instead of evaporation of seawater. Whether a lake becomes salty or not depends on whether the lake lacks an outlet and the relative balance between the inflow and outflow of lake waters via evaporation. Ocean water accessing a continental lake as the result of a single catastrophic event, as Tollmann's hypothesis proposes, would contain an inadequate amount of dissolved minerals to produce, when evaporated, the vast quantities of salts and other evaporites found in the salt lakes, flats, and pans cited as evidence of a mega-tsunami by this hypothesis.

Geological criticism

Isostatic rebound

Many published papers demonstrate that isostatic depression of the Earth's crust happened in the early Holocene. This process has led to submerging substantial portions of coastal areas adjacent to continental ice sheets and resulted in the accumulations of marine sediments and fossils within them. A well-documented example of flooding caused by isostatic depression is the case of Charlotte, The Vermont Whale, a fossil whale found in the deposits of the former Champlain Sea. As with many similar marine deposits, the sediments which accumulated within the Champlain Sea lack the physical characteristics—sedimentary structures, interlayers, and textures—that characterise sediments deposited by a mega-tsunami. These deposits and the associated fossils have been dated to significantly earlier periods than the times the bolide hypothesis proposed. In the case of the Champlain Sea, its sediments started to accumulate around 13,000 BP, almost 3,400 years before the oldest of the hypothesized Holocene bolide impacts.

Dating

A significant amount of the physical evidence used by Kristan-Tollmann and Tollmann, as supporting their hypothesis, is either too old or too young to have been created by this hypothesized impact. In many cases, it is hundreds to thousands, and in one case hundreds of thousands, of years too old to be credible evidence of a Holocene impact. The research that dates the tektites, which Tollmann's bolide hypothesis regards as indicative of the timing of the impact, is outdated. Later research, has dated the Australasian tektites to the Middle Pleistocene; about 790,000 years BP. In addition, the formation of salt lakes and salt flats is neither synchronous nor consistent with the hypothesized impacts having occurred about either 9,640 BP or 5,150 BP. For example, in the case of Lake Bonneville, Lake Lahontan, Mono Lake, and other Pleistocene pluvial lakes in the western United States, the transition to salt lakes and salt flats occurred at different times between 12,000 and 16,000 BP. Thus, the change from freshwater to salty water and eventually salt flats started over 2,400 to 6,400 years before the oldest of the impacts hypothesized by the Tollmann bolide hypothesis occurred. As a result, it is impossible that the formation of these salt lakes could have been associated with the impact hypothesized by Kristan-Tollmann and Tollmann.

Megatsunami

… excerpt ends here. Continue reading the full article.

Illustrations

Tollmann's bolide hypothesis: Isostatic rebound in the British Isles
Isostatic rebound in the British Isles
Tollmann's bolide hypothesis: Lake Bonneville and other ice age pluvial lakes (17,500 years BP), and modern remnants
Lake Bonneville and other ice age pluvial lakes (17,500 years BP), and modern remnants
Tollmann's bolide hypothesis: The megatsunami-producing Storegga Slide in Norway has been dated to approximately 6225–6170 BCE
The megatsunami-producing Storegga Slide in Norway has been dated to approximately 6225–6170 BCE

Worked examples

Example 1 — a first encounter with Tollmann's bolide hypothesis

Start with the simplest possible case. Write down what Tollmann's bolide hypothesis 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 Tollmann's bolide hypothesis 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 Tollmann's bolide hypothesis 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 Tollmann's bolide hypothesis

In research
Tollmann's bolide hypothesis 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 Tollmann's bolide hypothesis 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
Tollmann's bolide hypothesis is common in secondary-school and first-year university syllabi. It links to neighbouring topics Extinction events, Historical geology, Hypothetical Earth impact events, so understanding it makes those chapters shorter.
In everyday life
Look for Tollmann's bolide hypothesis 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 Tollmann's bolide hypothesis in 20 minutes

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

Frequently asked questions

What is Tollmann's bolide hypothesis in simple terms?

Tollmann's bolide hypothesis, proposed by Austrian palaeontologist Edith Kristan-Tollmann and geologist Alexander Tollmann in 1994, holds that one or more bolides struck the Earth around 7640 ± 200 BCE and that a smaller impact occurred around 3150 ± 200 BCE. The hypothesis proposes that the impact…

Why does Tollmann's bolide hypothesis 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 Tollmann's bolide hypothesis?

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 Tollmann's bolide hypothesis.

Tags

  • Extinction events
  • Historical geology
  • Hypothetical Earth impact events

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