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1839 Coringa vs. 1815 Mount Tambora - Comparison of...
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1839 Coringa vs 1815 Mount Tambora

1839 Coringa
1815 Mount Tambora
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1839 Coringa

Total costsN/A
Deaths 300000

Informations

On 25 November 1839, the port city of Coringa in Andhra Pradesh on the southeastern coast of British India was battered by a tropical cyclone that destroyed the harbor. Known as the 1839 Coringa cyclone and sometimes also referred to as the 1839 India cyclone and 1839 Andhra Pradesh cyclone, its storm surge caused wide damage. It killed over 300,000 people, making it the second-deadliest storm worldwide after the 1970 Bhola cyclone. Many ships were destroyed and houses were washed out by rising rivers and streams. Croplands were inundated and many animals drowned due to the floods and storm surge. The port city was not rebuilt after the cyclone. Some individuals who survived the disaster rebuilt their homes far from the coast. Some British officials named the area Hope Island, hoping to protect the city from future environmental disasters.

Source: Wikipedia
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1815 Mount Tambora

Total costsN/A
Deaths 250100

Informations

The 1815 eruption of Mount Tambora was the most powerful volcanic eruption in recorded human history, with a Volcanic Explosivity Index (VEI) of 7. The eruption ejected 160–213 cubic kilometres (38–51 cu mi) of material into the atmosphere. It is the most recently known VEI-7 event and the most recent confirmed VEI-7 eruption.Mount Tambora is on the island of Sumbawa in present-day Indonesia, then part of the Dutch East Indies. Although its eruption reached a violent climax on 10 April 1815, increased steaming and small phreatic eruptions occurred during the next six months to three years. The ash from the eruption column dispersed around the world and lowered global temperatures in an event sometimes known as the Year Without a Summer in 1816. This brief period of significant climate change triggered extreme weather and harvest failures in many areas around the world. Several climate forcings coincided and interacted in a systematic manner that has not been observed after any other large volcanic eruption since the early Stone Age.

Source: Wikipedia

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