📘 A mountain became a six-kilometre hollow
Stand on Tambora's rim: the summit is gone. A six-kilometre caldera occupies the top of the former mountain, the footprint of an eruption that transformed Sumbawa and sent sulfur high into the atmosphere.
What you’ll learn
- Tambora breaks the shape of an islandExplain how the 1815 Tambora eruption formed a caldera and why its deposits reveal exceptional scale.Tambora's missing summit and enormous deposits preserve the local geology of a global event.
- Krakatoa turns eruption into tsunamiCompare Krakatau's 1883 collapse, tsunami, and rebuilding with Tambora's island-scale destruction.Krakatau shows how a volcano's coastal geography can turn eruption into a tsunami disaster.
- Sulfur changes the skyTrace sulfur dioxide from an eruption to sulfate aerosols, reduced sunlight, and uneven cooling.The climate effect comes from atmospheric chemistry and circulation, not ash alone.
- 1816 makes weather historicalConnect 1816 weather anomalies to harvests, institutions, records, and cultural responses without oversimplifying causation.The Year Without a Summer became history through the interaction of climate and human vulnerability.
Questions this course answers
What made Tambora's caldera so broad?
A very large eruption removed material and allowed the summit roof to collapse.
Why was Krakatau's setting important?
The Sunda Strait let displaced water and volcanic flows threaten coastal communities.
Which material drove Tambora's longer-lived climate effect?
Sulfate aerosols scatter sunlight and alter atmospheric radiation for months to years.
What does Year Without a Summer mean?
The name describes widespread seasonal anomalies, not a uniform permanent winter.
Why do historians use several kinds of evidence for 1816?
Geology, observations, models, diaries, and prices answer different parts of the causal story.
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