📘 At the edge of a vanished summit
Stand at Tambora's rim on Sumbawa and look into a six-kilometre-wide absence. The mountain you see is not simply an unusually large crater: it is a caldera, formed when the summit collapsed after the enormous April 1815 eruption removed sup
What you’ll learn
- Tambora changes the mountainExplain how the 1815 eruption changed Tambora's shape and how geologists reconstruct its scale.The caldera, deposits, precursors, and pathways preserve local evidence of a globally important eruption.
- Krakatau turns water into a hazardCompare Krakatau's 1883 eruption with Tambora by tracing geography, displacement, and exposure.Krakatau shows how a volcanic island beside populated coasts can turn water and collapse into immediate danger.
- Sulfur makes a longer shadowTrace sulfur dioxide from an eruption to sulfate aerosols, sunlight reduction, and uneven climate response.Atmospheric chemistry gives a large eruption influence that lasts beyond the visible ash cloud.
- 1816 makes weather historicalConnect the 1816 climate anomaly to harvests, evidence, vulnerability, and cultural response without oversimplifying causation.The Year Without a Summer became history through the interaction of climate and human systems.
Questions this course answers
What produced Tambora's broad caldera?
The huge eruption removed and fractured material, allowing the summit roof to collapse.
Why did Krakatau's location matter?
The Sunda Strait let displaced water and volcanic flows threaten coastal communities and ships.
Which material drove the longer-lived climate effect?
Sulfate aerosols can spread through the stratosphere and reflect sunlight for several seasons.
What does Year Without a Summer mean?
The phrase describes widespread seasonal anomalies, not a uniform permanent winter.
Why compare diaries, prices, and climate records?
Different evidence types illuminate different parts of the eruption-to-society chain.
Grounded in trusted sources
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